"geology" Archives | Browse Articles & Resources Written By Experts https://usenaturalstone.org/tag/geology/ Articles & Case Studies Promoting Natural Stone Fri, 12 Jul 2024 19:51:34 +0000 en-US hourly 1 https://usenaturalstone.org/wp-content/uploads/2019/07/cropped-use-natural-stone-favicon-2-1-32x32.png "geology" Archives | Browse Articles & Resources Written By Experts https://usenaturalstone.org/tag/geology/ 32 32 Coming Full Circle with Super White https://usenaturalstone.org/coming-full-circle-with-super-white/ Fri, 12 Jul 2024 19:51:24 +0000 https://usenaturalstone.org/?p=11681 My involvement with the natural stone industry began in a distinct moment in 2012. In the midst of a kitchen remodel, I was browsing kitchen discussions on the Houzz website, learning about grout and cabinet hinges and numerous other topics that suddenly were of urgent importance.

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Coming Full Circle with Super White

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My involvement with the natural stone industry began in a distinct moment in 2012. In the midst of a kitchen remodel, I was browsing kitchen discussions on the Houzz website, learning about grout and cabinet hinges and numerous other topics that suddenly were of urgent importance. 

Then a fascinating thread scrolled into view, asking, Anyone ever cover their marble with saran wrap for a party? I eagerly clicked into the lively discussion about a Super White countertop that had been etching unexpectedly. Would covering it in plastic wrap be a good solution? The resounding answer was no, it would not.

At that time, Super White was still relatively new on the scene and often mislabeled as a quartzite, leading to disappointment when it didn’t act like one. Hence, the urge to wrap it in plastic.

On my next visit to the slab yard, I spotted a slab of Super White. Swoon! That’s one gorgeous stone – a blend of white and cool greys arranged in a dynamic pattern reminiscent of a fractured ice floe. It was immediately obvious why the stone was a superstar, despite the nebulous problem with its identity.

The helpful salesperson gave me a sample and I went home to do some diagnostics. The stone didn’t scratch glass, which ruled it out as a quartzite. I put a single drop of diluted hydrochloric acid on the stone, expecting a slight fizzing action and an etch mark. But nope, the stone didn’t etch. That meant it wasn’t a calcite-based marble. Next up, the test for dolomite: I roughed up an area of the stone with a nail, then put a drop of acid on the bits of powdered rock I’d scraped up. Bingo! It fizzed – the stone is made of dolomite.

Dolomite is similar to calcite but it contains some magnesium in addition to calcium. Compared to calcite, dolomite is slightly harder and it etches more slowly. That makes a dolomitic marble somewhat more durable than “regular” marbles that are made entirely of calcite, but the difference is subtle. 

There’s one more complicating factor with identifying Super White. The rock has fractures that are filled with quartz. This happens when the rock breaks underground – usually due to some sort of tectonic stress – and then mineral-rich groundwater fills in the broken parts. Geologists call this texture a “breccia” and it’s what gives Super White its magnificent pattern of white marble fragments floating in a river of grey. These small areas of quartz may have led to the stone being mislabeled as a quartzite, but it’s not a quartzite by any stretch. The rock’s full scientific name is brecciated dolomitic marble. 

Marble is a stone that’s been beloved and useful through the ages, but it’s one that warrants careful consideration. The potential for etching and scratching can be a dealbreaker for some, but no problem for others – but either way, people need to be able to make an informed decision. The more that sales reps, fabricators, designers, and homeowners can learn about the properties of stone they’re considering, the happier everyone will be. 

I wrote up my findings in a post on Houzz in a thread called The lowdown on Super White, and woke up the next morning to find a half-dozen responses and questions. By the time I’d answered the follow up questions, several more appeared. Who knew that geologic descriptions of countertop stones would be such a hit? The thread soon reached its 150-post limit so I started another. It too quickly filled up so I started yet another, and another. I’d unexpectedly stumbled into a topic that seemed a good match for a geologist who happens to like kitchens.

Before too long I’d found the Marble Institute of America (now the Natural Stone Institute) and a happy collaboration was born. One of our first priorities was to delve into this very topic: The Definitive Guide to Quartzite. The popularity of marble and quartzite led to articles such as Telling White Stones Apart, that aimed to help people sort out the differences between similar-looking stones.

But there was one more element of that original post that was prescient. I wrote, “I swoon every darned time I pass by a slab of white marble. I just love it! But I will have to come up with another place to use it, like as a mantle or a countertop on a china cabinet.”

Fast-forward 12 years, and my dream built-in cabinet and bookcase was being installed, and I could finally carry out that vision. I still stop dead in my tracks every time I come face to face with a slab of white marble. It’s an exquisite material, made all the better because it comes naturally from the Earth. At last, I was admiring these beauties as a customer, not a scientist.

I checked out many different slabs, but honestly, there was never a doubt in my mind that I’d end up with Super White. It also happened to be the only white stone that my husband liked. I was able to find a remnant piece with a brilliant pattern of fracturing that was gloriously similar to the satellite images of sea ice that I use in my science writing for NASA. I stood in front of the slab and ran my fingers over the leathered surface, appreciating the texture of the marble blocks floating within the icy quartz veins. I felt so very lucky that it was finally time for a piece of glorious white stone of my own.

 

Can you tell which image is Super White and which is the spring breakup of Arctic Sea ice? The image on the left is Super White, and is about 10 inches across. The one on the right is a NASA satellite image of Baffin Bay from April 18, 2024, and it’s around 150 miles across.

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Telling White Stones Apart https://usenaturalstone.org/telling-white-stones-apart/ Fri, 10 Apr 2020 20:23:11 +0000 https://usenaturalstone.org/?p=7575 White stones are popular, frequently mislabeled, and often misunderstood. Learn how to tell if your white stone is a granite, quartzite, or marble. White stones are popular, frequently mislabeled, and often misunderstood.

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Telling White Stones Apart

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How to Tell If Your White Stone is a Granite, Quartzite, or Marble

One of the favorite parts of my job as a roving geologist is to share not just an appreciation for natural stone, but a deeper understanding of it. With a little guidance and practice, anyone can learn to recognize the properties and aesthetics of various types of stone. No matter a slab’s label, country of origin, or price tag, some basic geologic savviness can help us understand it better.

The process of identifying stones gets most confusing when they look alike, and nowhere is this more vexing than with white stones, which are popular, frequently mislabeled, and often misunderstood. But fear not. Even similar-looking stones can be sorted out by using a few basic guidelines.

Read on, as we step through the process of differentiating light-colored granites, quartzites, and marbles.

Granite has a distinct look, compared to quartzite and marble.

Granite is the most common type of natural stone in the trade and comes in a satisfyingly large range of colors and patterns. Despite their diverse aesthetics, granites have common elements that make them recognizable. Below are some rules of thumb. Please note that I’m referring to the general industry classification of granite, rather than the narrower geologists’ definition.

  • Light colored granites have flecks or blocks of varying colors. White granites are rarely a homogeneous, even-toned color. Most light colored granites have more than one color in them, and it’s rare to have a white granite without any darker minerals at all.

  • Individual minerals are visible. Look for blocky crystals of feldspar, glassy areas of quartz, and a smattering of darker colored minerals. Learn more about what different minerals look like.
  • Sometimes granite has giant minerals! If the slab has minerals larger than couple of inches, then you’ve got a pegmatite. That’s special type of granite with super-sized crystals. Patagonia is one of the more dramatic examples of a granite pegmatite, and Tourmaline, Alpine, Alaska White, and Delicatus are other examples.
  • If it contains garnet, it’s granulite or gneiss. Garnets are small, round minerals that are dark pink, burgundy, or reddish brown in color. Their presence is an instant giveaway that you’re looking at metamorphic variations of granite. Gneiss has stripes or bands of lighter and darker minerals, while granulite tends to have few or no stripes and is generally light colored overall. There are many white granulites on the market, including Bianco Romano, Colonial White, or Giallo Cream. Viscount White is an example of gneiss.
  • Mica is common in granite. Mica is present in small amounts in granite, and it makes an appearance as glittery minerals that can be silver, gold, bronze, or metallic black. If a stone is mostly made of mica, then it’s schist.
  • Granite can have quiet patterns or vivid movement. Leave it to Mother Nature to create waves of color, veins of contrasting minerals, and all sorts of other interesting effects. That’s a big part of the appeal of a natural stone.
  • Read more about the variations, colors, and origins of granite.

 

Marble and quartzite look different from granite, but similar to each other.

Marble and quartzite look alike in several ways.

  • They tend to be mostly light colored: white, light grey, cream. Darker colors are also possible.
  • Marble and quartzite are usually fine grained overall; you can’t put your finger on an individual mineral grain.
  • They often have layers or bands of contrasting colors. The layering can be straight, wavy, or chaotic.
  • Slabs can have quiet patterns or vivid movement.
  • If a slab has fossils, then it’s limestone, not marble. Limestone has a chalky or matte finish compared to either marble or quartzite.
  • Read more about marble and quartzite.

To tell marble from quartzite, check their properties.

 The fact that these two stones look alike is why they are so frequently mislabeled and misunderstood. Your best bet is to rely on the way the stones behave rather than how they look. Thankfully, marble and quartzite have consistent traits that you can use to tell them apart.

  • Quartzite is much harder than marble and slightly harder than granite.
    You can use a glass tile or a knife blade to gauge the hardness of a stone. Quartzite will leave a definite scratch on glass, and a knife blade will not easily scratch the stone (though it may leave a silvery mark on the stone, which is the metal rubbing off on the stone). Learn more about identifying quartzite in the Definitive Guide to Quartzite.

  • Marble is relatively soft.
    A knife blade will make obvious scratch marks on marble; and marble will not scratch glass. Some marbles, like Super White or Fantasy Brown, may have isolated pockets of quartz amid an overall composition of marble. When in doubt, check a few different areas of the stone.
  • Quartzite is not affected by acids.
    Vinegar, lemon, wine, citrus, or any other common acid won’t affect quartzite. Strong chemicals like oven cleaner or rust remover can damage almost any stone, though, so be careful with those.
  • Marble is acid-sensitive.
    The mineral calcite is dissolved by acids, and many types of stone contain calcite, such as limestone, onyx, travertine, and marble. (Science trivia: this is why acid rain caused damage to buildings and monuments before we got a handle on the pollution that causes acid rain.) Dolomite is a mineral that is chemically similar to calcite, and it’s also affected by acids but not as quickly. In either case, acids leave an etch mark or a dull spot on the surface of the stone. Etches do not affect the structural integrity of a stone, and they can be polished out if need be. For people who love marble, etches are often considered a part of the living surface of the stone, which develops depth and character over time. If that idea makes you cringe, then you know marble is not for you. Choose quartzite or granite instead!

Granite, marble and quartzite can be porous…or not.

Some types of stone have small pore spaces within the stone, and a porous stone can absorb liquids and become stained. There are several geologic processes that affect a stone’s porosity. For example, if a stone does not get buried too deeply when it forms, tiny spaces can remain between mineral grains. Another possible cause of porosity is underground fracturing along fault lines where rocks grind up against each other. Sometimes groundwater dissolves away pieces of the stone. On the other hand, groundwater can also do the opposite – it can add bits of minerals that will fill in pore spaces.

So we just have to live with the fact that sometimes granite, marble, and quartzite are slightly porous, and sometimes they are not. That also means that porosity cannot be a guide to helping us identify a stone. We can’t say that a stone is porous therefore it’s marble, for example. Because plenty of marbles are dense and impermeable. The same is true for granite and quartzite, too.

The porosity of quartzite can be especially confusing, and you can learn more in the Deep Dive Into the Properties of Quartzite.

So while rules of thumb fail us, what we can do is test slabs to learn about their porosity – which is actually ideal, because you’ll get specific details on the slabs of interest.

Refer to How to Be Your Own Stone Sleuth for instructions and photos showing how to test your slab’s hardness, acid sensitivity, and porosity. Nothing can beat the hands-on information you’ll get from doing a little “sciencing” on various slabs, and it’s pretty fun, too.

So don’t let the array of white stones get the better of you. By learning a bit more about how different stones get their particular aesthetics and properties, you’ll be able to enjoy them all the more.

More from the Geology Series

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How to Be Your Own Stone Sleuth https://usenaturalstone.org/how-to-be-your-own-stone-sleuth/ Thu, 20 Feb 2020 23:05:57 +0000 https://usenaturalstone.org/?p=7405 Learn how to test stone samples for hardness, acid resistance, and porosity. Kitchen designers, architects, fabricators, and restoration professionals can use diagnostic techniques to learn as much as they can about particular varieties of natural stone.

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How to Be Your Own Stone Sleuth

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Test your slabs for hardness, acid resistance, and porosity

 

Many of my articles extoll the virtues of using simple tests to learn more about the properties of natural stone. So I get a kick out of hearing about customers arriving at stone showrooms armed with lemon slices, pocketknives, glass tiles, and notebooks, ready to perform an impromptu geology lab on their natural stone. It goes without saying that these tests need to be carried out with the blessing and cooperation of the sales staff, but I’m totally in favor of this trend. Similarly, I encourage salespeople, kitchen designers, architects, fabricators, and restoration professionals to use diagnostic techniques to learn as much as they can about particular varieties of natural stone. Information gleaned from these tests helps us all.

With that said, let’s break out the tools, roll up our sleeves, and do some stone sleuthing!

 

Test for hardness

When taking stock of a stone’s properties, it’s wise to start with hardness. This simple, flexible test can tell you a lot about a stone.

  • Find a sharp, broken edge of the stone.
  • Place a glass tile on a tabletop, and then press the pointed edge of the stone into the glass.
  • Drag the stone along the glass, pressing firmly, but no so hard that you risk breaking the glass.
  • Then inspect the glass. Did the stone leave a true scratch that you can feel? Or did the stone simply ‘draw’ on the glass?
  • Usually when the stone is scratching the glass you can feel and hear it biting in. When the stone is softer than the glass, it almost feels slippery as it glides across the surface.

If you don’t have a small sample, you can test a full slab:

  • If you don’t already own the slab, make sure you get permission before doing this!
  • Use the tip of a pocketknife, an awl, or similar pointy metal tool.
  • Press firmly and drag the tool back and forth across the surface of the stone.
  • Most of the time the tool will leave a mark, and you’ll need to determine what the mark is. If it’s a scratch, it will work up small amounts of powdered rock, and make a visible indentation in the stone.
  • The tool can also rub off on the stone, leaving a silvery or light-colored mark – the key difference is that you can rub this mark off and there will be no indentation left behind.
  • Repeat the test multiple places, particularly if the slab is made up of different minerals or colors.
  • Sealer will have no effect on hardness tests.

What the results mean:

  • Granite, gneiss, sandstone, and quartzite will all scratch glass and will not be significantly scratched by a metal tool.
  • Marble, dolomitic marble, limestone, travertine, onyx, soapstone, and serpentine will not scratch glass. A metal tool will scratch these types of stone.
  • This test can also reveal how a stone responds to being scratched, poked, and prodded. Does it flake apart at the edges? Do grains pop out? Does it chip? Be on the lookout for clues about how the stone tends to break.

 

Test for acid sensitivity

Use this test to distinguish a potentially mislabeled quartzite from marble, and to get a sense of how a particular stone will respond to common acids.

  • Put several large drops of lemon juice or vinegar on the surface of the stone and leave it there for 5-10 minutes.
  • Sometimes you can see a faint bubbling or fizzing on an acid-sensitive stone, but you might have to use a magnifier to see this.
  • Wipe down the stone and look at it at a low angle. Etched areas can look dulled, as if the stone’s polish has been removed.
  • Polished slabs typically will have more noticeable etching than honed or leathered slabs.
  • Sealers do not protect a stone from interactions with acid, so this test can be done on a sealed or unsealed sample.

What the results mean:

  • Stones that contain calcite or dolomite will etch from contact with common acids.
  • Marble, limestone, travertine, and onyx are all made of calcite. Dolomite is a similar mineral that etches somewhat more slowly. Super White is made of dolomite, for example.

 

Test for porosity

This test is best done on an unsealed sample so you can assess the stone’s true porosity, but if you want to test the effectiveness of a sealer, you can do the second or third variations of test with a sealed stone.

If you have a small sample of the stone:

  • Fill a shallow bowl with water and place the stone, edge-wise, in the water so only part of it is submerged in the water. You can also do this test with some food dye in the water, which can make the results easier to see.
  • Leave for 10-15 minutes, then remove from the water and dry thoroughly. Let the stone air dry for about 10 minutes so that the surface of the stone becomes dry. Then you can evaluate if water worked its way inside the stone.
  • Inspect the stone to see if water has wicked up into the stone above the water line. If so, the stone might be more prone to staining after installation.
  • Then check to see if the stone looks darker below the water line. If so, it’s moderately porous.
  • If the stone has not darkened, then it absorbed little to no water and it has low porosity.

On a full slab, in the horizontal position:

  • If you don’t already own the slab, make sure you get permission before doing this!
  • Dribble water onto the surface and leave for 10-15 minutes.
  • Wipe up the water and dry thoroughly. Let the stone air dry for about 10 minutes.
  • A darkened area indicates that the stone has absorbed water.

On a full slab, in the vertical position:

  • If you don’t already own the slab, make sure you get permission before doing this!
  • This is the least helpful way to gauge porosity, but sometimes it’s the only option.
  • Use a spray bottle to spritz water on the surface of the slab. The water will run off, but you will be able to observe how water interacts with the stone. Does the water leave a darker shadow, or does it bead up and run off entirely?
  • If you have access to a broken edge of the stone, put water there and see what happens.
  • Another option is to drape a wet towel on the stone and leave it in place for 10-15 minutes.

What the results mean:

Porous stones are more likely to stain. Although porosity can be reduced with sealer, it’s still wise to consider a stone’s natural tendency to absorb liquids so that the sealer is not the only defense against staining. Ideally, avoid putting a porous stone in a place where it will have to endure a lot of liquids.

 

Diagnostic tests on stone samples can be fun and informative experiments, and they give you an up-close-and- personal sense of the behavior of a particular slab. The more knowledge you have, the more confidence you’ll gain in your decisions. While many variations of natural stone offer gorgeous aesthetics and versatile utility, understanding their differences will help you pinpoint which ones are right for different circumstances. When you align a stone’s properties with the ways it will be used, the stone itself can take center stage, for many years to come.

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A professional-level stone diagnostics kit can be purchased through MB Stone Pro: https://www.mbstonepro.com/products/stone-id-kit

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Natural Quartzite and Engineered Quartz: What’s the Difference? https://usenaturalstone.org/natural-quartzite-and-engineered-quartz-whats-the-difference/ Fri, 06 Dec 2019 17:48:56 +0000 https://usenaturalstone.org/?p=7305 Engineered quartz and natural quartzite are both popular choices for countertops, backsplashes, bathrooms, and more. Here’s a quick and handy reference for understanding where they come from, what they’re made of, and how they differ.

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Natural Quartzite and Engineered Quartz: What’s the Difference?

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Engineered quartz and natural quartzite are both popular choices for countertops, backsplashes, bathrooms, and more. Their names are similar, and are sometimes (incorrectly) used interchangeably. But even aside from the names, there’s a lot of confusion about these materials.

Here’s a quick and handy reference for understanding both engineered quartz and quartzite: where they come from, what they’re made of, and how they differ.

 

Quartzite is a natural stone.

Quartzite is 100% natural and comes directly from the earth. Quartzite has formed in locations all around the planet and the most well-known quartzite quarries are in Brazil. Quartzite is also quarried in the United States, Sweden, Canada, Norway, India, and Italy, among other locales. Dramatic settings like the Medicine Bow Mountains in Wyoming show off quartzite in its natural habitat, where an impressive massif of white quartzite rises above the surrounding terrain.

Medicine Bow Peak in Wyoming is made from white quartzite that is over a billion years old. Photo: Wikimedia Commons by Fredlyfish4.

 

Engineered quartz is manmade.

Even though the name “quartz” refers to a natural mineral, engineered quartz (sometimes also called “engineered stone”) is a manufactured product. It’s made from quartz particles bonded together with resin, pigments, and other ingredients. Manufactured quartz is made in factories in the United States, Europe, and Asia, among other locations.

 

Natural quartzite contains minerals, and nothing else.

All quartzites are made of 100% minerals, and are purely a product of nature. Quartz (the mineral) is the main ingredient in all quartzites, and some types of quartzite contain smaller amounts of other minerals that give the stone color and character. The diverse options in aesthetics are impressive—and all from the earth. So if you like calm monochrome, nature provides that. If wild streaks of color tug on your heart, nature’s got you covered.

Some examples:

 

Engineered quartz contains minerals, polyester, styrene, pigments, and tert-Butyl peroxybenzoate.

The exact blend of ingredients in engineered quartz varies by brand and color, and manufacturers tout the high percentage of minerals in their slabs. The oft-cited statistic is that manufactured quartz contains 93% mineral quartz. But there are two caveats. First, 93% is the maximum, and actual quartz content can be much lower. Secondly, that percentage is measured by weight, not volume. A particle of quartz weighs a lot more than a particle of resin. So if you want to know how much of a countertop surface is made of quartz, then you need to measure the ingredients by volume, not weight. Based on proportions of materials in PentalQuartz, for example, the product is around 74% mineral quartz when measured by volume, even though it’s 88% quartz by weight.

 

Quartzite is made from geologic processes, over millions of years.

Some people (me included!) love the idea of having a slice of geologic time in their home or office. Every natural stone is an expression of all of the time and events that shaped it. Each quartzite has its own life story, but many were deposited as beach sand, and then buried and compressed into solid rock to make sandstone. Then the stone was pushed deeper into Earth’s crust where it was further and compressed and heated into a metamorphic rock. During metamorphism, quartzite experiences temperatures somewhere between 800° and 3000° F, and pressures of at least 40,000 pounds per square inch (in metric units, that’s 400° to 1600° C and 300 MPa), all over the course of millions of years.

Natural quartzites are not all alike. There is variation in how deeply they were buried and for how long, and what types of conditions they endured. Because of this, some quartzites are somewhat porous (like Macaubus), while others are tightly bonded together (like Marine Blue, Taj Mahal, or Fusion). For an explanation of the different members of the quartzite family, check out A Deep Dive Into the Properties of Quartzite.

 

Engineered quartz is made in a mold.

Many quartz brands are made with the patented Breton process, which involves pouring the ingredients in slab-shaped molds, then subjecting the mixture to a vacuum, vibration, and pressure. In the words of the manufacturer, it’s called “compaction by vibrocompression vacuum process.” The Breton process compresses slabs at around 30 pounds per square inch, and applies heat up to 360° F for around 40 minutes (in metric, that’s 180° C and 0.2 MPa). For comparison, that’s about the same amount of pressure in a car tire, and the same temperature and duration as if baking a casserole. Then the slabs are cured in a kiln, cooled, and polished. Compared to nature’s way of making stone, this is certainly quicker and more controlled, but the amount of heat and pressure used to manufacture a slab are far less than what happens in nature.

Because quartz particles are encased in resin, engineered quartz ends up having low porosity even though it is not compressed as much as natural quartzite (water absorption up to 0.02% in weight, according to Breton). On the other hand, the presence of resin means that engineered quartz is softer than natural quartzite.

 

Quartzite can be used indoors and out.

Natural quartzite is at home in many applications, from countertops and flooring, to outdoor kitchens and cladding. Harsh weather and UV light won’t affect the stone.

 

Engineered stone is best left indoors.

As I learned when I left several quartz slabs outside for a few months, the resins in engineered stone will turn yellow in the sunlight.

 

Quartzite is often misunderstood.

An unfortunate side effect of the desirability of quartzite is the temptation to sell stones as quartzite when they are not quartzite. Thus, quartzite is commonly mislabeled, which has resulted in widespread confusion about the properties of the stone. So-called “soft quartzite” is usually marble, which has entirely different properties than real quartzite. Simple diagnostic tests can be used to differentiate quartzite and marble. Furthermore, some sandstones are sold as quartzite, which further adds to the mix-up. Sandstone and quartzite have the same mineral ingredients (quartz), but quartzite has much lower porosity, as is explained in the Deep Dive into the Properties of Quartzite. Thankfully, it seems that both industry pros and consumers are becoming more discerning about what quartzite truly is, or is not.

 

Engineered quartz is misunderstood, too.

One well-known brand of manufactured quartz literally calls itself natural stone, which it isn’t. Manufactured quartz is sometimes thought to be maintenance free, which would be nice, but engineered surfaces are not immune to staining, chipping, scratching, or damage from excessive heat. Just as with any other material, users of manufactured quartz surfaces need to be mindful of the properties of engineered quartz and the particular requirements for its care.

Some misconceptions about engineered quartz are addressed in Sifting Through the Confusion about Manmade Quartz Surfaces and Do Engineered Quartz Countertops Stain?

 

Quartzite needs sealing.

The most common problem with quartzites is inadequate sealing – particularly along the edges and cut surfaces. As described above, some quartzites are porous and care must be taken to seal the stone. When in doubt, be sure to work with a fabricator who is experienced with the particular quartzite you are considering.

 

Engineered quartz should be protected from heat and not scrubbed too hard.

In a series of tests, major brands of engineered quartz stood up reasonably well to staining, but were damaged by scrubbing with abrasive cleaners or scouring pads. Exposure to hot, dirty cookware damaged some types of quartz, as was shown in a performance comparison of countertop materials.

 

Which should you use?

There is no simple answer to this question. Each material has its devoted fans and selling points. No matter which surface you choose, be sure to obtain samples that you can test, work with a reputable dealer and fabricator, and take some time to learn about the product. While labels and misconceptions can cause confusion, the combination of informed customers and experienced professionals can help ensure that materials are used in ways that allow them to perform well, last a long time, and look terrific every day.

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Know Your Minerals https://usenaturalstone.org/know-your-minerals/ Fri, 30 Aug 2019 20:01:47 +0000 https://usenaturalstone.org/?p=7095 Minerals are the components of all natural stones. The color of every natural stone, whether it’s jet black, glittery silver, or a kaleidoscope of Technicolor – comes from the individual minerals. Read more in this handy guide to the ingredients of your favorite natural stone.

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Know Your Minerals

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Our thanks to Slabworks of Montana and Montana Tile and Stone for allowing us to explore and photograph their beautiful stone slabs.

 

A handy guide to the ingredients of your favorite natural stone

Minerals are the components of all natural stones. The color of every natural stone, whether it’s jet black, glittery silver, or a kaleidoscope of Technicolor – comes from the individual minerals.

Minerals also give each stone its personality. Is it flashy, or subtle? Is it a uniform color, or a melee of diverse ingredients?

And, of course, minerals dictate the properties of a stone: Hard or soft; acid-resistant or acid-sensitive; flaky, chunky, or smooth.

Given that minerals determine so much about a stone, it warrants a look at some of the more common minerals, how to spot them, and what they tell you about a stone.

Before we dive in, one important point is that you can only see individual minerals in coarse-grained stones. A smooth stone with small grains, like Absolute Black or Pietra Grey, doesn’t reveal much about specific minerals because you can’t see them. But many popular stones have big crystals in all kinds of patterns and colors, inviting curiosity about just what those minerals are all about. 

 

Feldspar

Feldspar is the most abundant mineral in the Earth’s crust, but it’s far from mundane because it occurs in a huge range of colors and forms. When you look at a slab of typical granite, you’re looking at mostly feldspar. Igneous rocks like granite take shape as they solidify from liquid magma. You can think of magma as a ‘slushy’ drink. It’s a mixture of solid bits and liquid. Feldspar crystals are often the solid chunks within a body of slushy magma, and you can see the chunky texture of feldspar in some granite slabs.

In other cases, feldspar is altered by metamorphism, changing its shape from pushing, pulling, or shearing. In these cases, the blocky shapes of feldspar crystals can become more rounded.

Color:

Feldspar crystals can be white, black, and any shade of grey. They can also be pink, cream, brown, and sometimes green. Best yet, the variety of feldspar called labradorite is iridescent blue, and plays the starring role in Blue Pearl and Volga Blue.

Identifying features:

Since feldspar can be nearly any color, using color to identify it won’t help at all. But it does have a few features that make it recognizable.

  • Feldspar is not glossy and its luster is similar to porcelain when it’s not polished.
  • It is always opaque, meaning, you can’t see ‘into’ the crystal at all.
  • It’s more or less rectangular in shape.
  • The crystals break into naturally flat faces called cleavage planes. This is especially visible on a honed or leathered slab when you look at it from an angle. The flat faces will catch the light. This is also evident on the edge of a slab where you can see a crystal in three dimensions.
  • You can sometimes see subtle stripes or grooves in a feldspar crystal.

Properties:

Feldspar is an all-around easygoing mineral. It has no special needs, has a Mohs hardness of 6 to 6.5 (harder than glass), and holds up well to hard use. It won’t etch, flake, or offend anyone in any way.

Examples: Alpine White, Antique Brown, Patagonia, Coral Grey, Blue Pearl, and many others. Since feldspar is such a common mineral, there are dozens of examples.

Superpower: Feldspar makes you more gracious and less self-involved. The relaxed flow of energy from feldspar allows you to let someone else take that last slice of pizza, even though you’re still a little bit hungry.

Quartz

Quartz is the second most abundant mineral on the Earth’s crust. Even though it occurs in similar colors as feldspar, it has a distinctly different look.

Colors: Clear, white, grey, black, pink, amber, brown, purple. Some colors of quartz have their own name. Purple quartz is amethyst. Amber quartz is citrine. Grey quartz is smoky quartz, and so on.

Identifying features:

Once again, color is no help in identifying quartz, but quartz is easy to spot once you see it a few times.

  • Quartz is often translucent, meaning you can see down into the crystal.
  • Quartz looks a lot like colored glass, because it has the same chemical composition as glass.
  • Unlike feldspar, quartz does not have a ‘preferred’ shape and it almost never breaks along a flat plane.
  • When looking at an igneous rock, quartz is often blob-shaped, because it’s the last mineral to solidify and it fills in the gaps left open between the other minerals.
  • In a metamorphic rock like gneiss, schist, or a quartzite like Fusion or Marine Blue, quartz forms white blobs that are often squiggly-looking. In these cases, the quartz melted as the rock was undergoing metamorphism.

Properties:

Quartz is heralded for being beautiful, durable, inert, and generally bombproof. It’s 7 on Mohs hardness scale and isn’t bothered by acids or less-than-ideal cleaning habits. In fact, quartz is such a cool mineral, that a type of manmade countertop material borrowed its name, leading to endless confusion within the countertop industry.

Examples: Quartz is prevalent in light colored granites like Alaska White or Bianco Antico. And, of course, quartz plays the starring role in quartzites like Taj Mahal, Fusion, and Sea Pearl. Quartz is also the main ingredient in Wild Sea sandstone.

Superpower: Having quartz-rich stones in your home makes you less likely to snack between meals. No one knows why.

[Disclaimer – these superpowers are not to be taken literally. Hopefully you already realized that?]

Garnet

Garnet is January’s birthstone, and it’s a beautiful mineral. Garnet is dark-raspberry pink, maroon, or maroonish-brown.

Identifying features:

  • The color is usually a total giveaway.
  • The crystal shape is usually round-ish. It often occurs in specks.
  • Garnet crystals have a glassy luster, and when viewed on the edge of a slab or in an un-cut rock, they are brilliantly sparkly.

Properties:

Garnet is 6.5 to 7.5 on Mohs scale and is often used as an abrasive. Large, translucent crystals of garnet are used for gemstones.

 

Examples: Garnet is not a major ingredient in any stone, but its recognizable crystals are in River White, Colonial White, Dallas White, and St. Cecilia, among others.

Superpower: People who like garnet are above average at math. Unfortunately, simply owning a garnetiferous stone will not, in and of itself, improve your math skills.

Mica

Mica is the defining ingredient in sparkling stones like Orion and Magma Gold, and is a minor player in granite and gneiss. Mica is nature’s glitter: it’s shiny and forms in flat flakes. It’s hard to identify mica in a polished surface, but if you look at the edge of the slab you can usually make out the trademark shape.

Identifying features:

  • When you view mica crystals end-on, you can see the very thin edges of the flakes. Sometimes these are stacked like pages in a book.
  • Mica sheets are pliable and you can likely bend them with your fingernail.
  • The mica family includes minerals of silvery white, golden, brown, and black. There is even a green mica called chlorite that gives green slate its color.

Properties:

Mica is best in small doses, because it’s soft and does not conform to polishing like other minerals. Small-grained mica is ideal because you can enjoy the sparkle without having the stone flake apart. Mica is a major ingredient in schist.

Examples: Many granites and gneisses have small amounts of mica minerals. Some examples include Delicatus White, Vahalla, Rocky Mountain, or Viscont White. Schists contain larger amounts of mica, as can be seen in Desert Dream, Galaxy Schist, or Saturnia.

Superpower: Mica makes you more tolerant of your family members.

Amphibole

Black flecks in an otherwise light granite are either amphibole or black mica. Amphibole and black mica are also the duo that makes up the dark stripes in gneiss. (The light stripes are feldspar and quartz.) Amphibole is also called hornblende.

Identifying features:

  • Amphibole is an even, jet black.
  • It tends to form crystals that are skinny rectangles, but sometimes it also has an irregular, blocky-ish shape.
  • You can tell the difference between mica and amphibole by shape. Mica = thin flakes, and amphibole = thin rectangles. It’s subtle, but different enough to be a reliable way to tell these minerals apart.
  • When in doubt, look at the edge of the slab to determine the crystal shape.

Properties:

Amphibole has a hardness between 5 and 6, which is similar to or slightly harder than glass. It takes a polish well, and does not need any special care. In most stones it’s a minor ingredient.

Examples: Amphibole is usually a minor ingredient in slabs, but it makes a spectacular appearance in Crowsfoot Schist, Montana Brown, and Alaska White. Stones like Barcelona, Roca Montana, and Bianco Antico have more subtle crystals of amphibole.

Superpower: Eases headaches; but also may cause cravings for salty things or Chinese food.

Calcite

This humble mineral expresses itself in so many wonderful ways. Calcite is the main ingredient in marble, limestone, travertine, and onyx.

Color:
Calcite is almost always white or nearly white, and it can have tones of other colors like cream, apricot, light brown, light green, light grey, or light pink.

Identifying features:

  • Calcite can look a bit like quartz (hence the perpetual confusion between marble and quartzite), but it has a few differences.
    • Calcite has a satin luster, while quartz looks glassy and is more translucent.
    • Calcite forms crystals with flat surfaces, and also breaks along flat planes. So when light reflects off calcite, you see glints of light from flat surfaces (see photo).
    • When in doubt, go by the properties rather than the looks.
  • Calcite is easily dissolved in groundwater and it often fills in cracks in rocks. Bright white stripes in dark colored limestone or marble are veins of calcite.
  • Just to make things more confusing, quartz can also make light colored veins in a stone. A quick hardness test with a pocketknife will reliably tell you which is which.

Properties:

The best way to tell calcite from quartz or feldspar is by its properties. Calcite has a Mohs hardness of 3, which is harder than a fingernail but softer than glass. A sharp-tipped nail or pocketknife will leave a definitive scratch in calcite. Also, vinegar dripped onto calcite will often gently fizz.

These same properties apply to slabs and tiles. Stones made of calcite can be etched from acids, and can also be scratched by metal or ceramic kitchen implements.

Examples: All marbles and limestones are made of calcite. Some well-loved examples are Carrara, Danby, White Cherokee, and Colorado White marbles; or Belgian Blue, Fossil Black, Saint Pierre, or Emperador limestones.

Superpower: Calcite makes it easier to keep world events in perspective and has been shown to reduce social media use.

Dolomite

This is calcite’s cousin, and shares similar color and properties of calcite with a few exceptions. Compared to calcite, dolomite is slightly less susceptible to etching from acids, giving you some time to wipe up spills before the stone is affected.

Identifying features:

  • Dolomite and calcite look alike and you can’t tell them apart visually.
  • The test for dolomite is called the ‘powdered rock acid test.’ Calcite will have a fizzing reaction when in contact with diluted hydrochloric acid. Dolomite will not, unless the stone is powdered first. To do this test, use a nail or tip of a knife and scratch up an area of the stone. Leave the stone dust in place, and then put one drop of acid on it. If the stone is dolomite, it will have a weak, bubbling reaction. If it’s some other type of mineral altogether, like feldspar, there will be no reaction at all.

Properties:

Dolomite has a Mohs hardness of 3.5, which is slightly harder than calcite. Dolomite also etches more slowly than calcite, but it will still etch.

Example: Super White a well known dolomitic marble that is frequently mislabeled as quartzite.

Superpower: Proximity to dolomite strengthens teeth and makes dental visits less stressful.

This is not a natural stone – it’s a slab of engineered quartz. One of the reasons manmade quartz does not look natural is because the ‘crystals’ are all blob-shaped and have the same luster. The recognizable rectangles of feldspar and glassiness of real quartz are absent.

QUIZ

Name these minerals:

 

A = quartz

B = feldspar

C = garnet

D = amphibole

More from the Geology Series

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Sifting Through the Confusion about Manmade Quartz Surfaces https://usenaturalstone.org/is-quartz-natural-stone/ Tue, 21 May 2019 20:39:09 +0000 https://usenaturalstone.org/?p=6233 Is quartz natural stone? Our geologist analyzed samples from several different quartz manufacturers. Sort fact from fiction using real scientific data to prove performance statistics.

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Sifting Through the Confusion about Manmade Quartz Surfaces

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Note: A version of this article appears in the Spring 2019 issue of Building Stone Magazine.

We are living in the age of information. In the palms of our hands, we can tap into an enormous realm of facts, opinions, advertisements, and educational materials. However, because information is so easy to access and share, plenty of not-so-great material gets widely circulated, too. Our challenge is to sort fact from fiction, to educate ourselves, and guide designers, architects, and customers through the melee.

The countertop industry is a big one, offering billions of dollars in annual sales in the United States alone. Naturally, competition is fierce as various companies vie for attention and make bold claims to lure customers. Quartz countertop manufacturers are working hard to influence the marketplace, and they are doing so with big promises and lofty assertions. As with all information, it’s important to pause and reflect on the validity of these statements so that we can make informed choices.

What’s In a Name?

Companies that manufacture quartz countertops have been very clever with their naming. The word “quartz” represents one of Earth’s most abundant minerals. One well-known brand of quartz surfaces says that their product is “pure natural quartz.” The phrase admittedly has a nice ring to it. But how accurate is it?

Geologically speaking, a manmade quartz countertop is not pure natural quartz. The only thing that fits that criterion is quartzite, which truly is pure natural quartz. Manufactured quartz surfaces are mostly quartz, but they are not purely quartz. Depending on the brand and the color, manmade quartz surfaces are 70% to 93% quartz sand or aggregate, mixed with polyester resin, ethenylbenzene (also known as styrene), pigments, and other additives.

Is Engineered Quartz the Same as Natural Stone?

I believe another area of confusion arises when quartz manufacturers refer to their products as natural stone. For example, one paragraph of a quartz company’s website begins: “All natural stone surfaces, including [company name]….” This type of phrasing is prevalent throughout the company’s marketing materials. In other examples, they say that they sell the world’s “most beautiful and innovative natural stone surfaces,” they “offer the world’s finest natural stone countertops,” and they describe their products as “stone slabs.”

From my perspective as a geologist and a professional admirer of rocks, I can easily appreciate the attempt to align a manmade product with a natural one. We can all agree that natural stone is awesome. But manmade quartz isn’t natural stone. It’s a bit brazen to say that it is. 

For the record, natural stone is both naturally occurring and made out of stone. Granite, limestone, quartzite, and marble are all natural stones. They form in nature, and only in nature. They are made of minerals, and only of minerals. Feldspar, quartz, hornblende, hematite, garnet, calcite, muscovite: these are the ingredients in nature’s pallet. You’ll find no polyester resin on a seafloor, nor ethenylbenzene in a magma chamber—thank goodness.

Will the Real Mont Blanc Please Stand Up?

Mont Blanc quartzite (right) a natural stone, is often imitated by manufactured quartz producers. Notice the inherent difference of one manufacturer’s Mont Blanc (left) and a second company’s Montblanc (center) as manufactured quartz product offerings compared to its natural counterpart. Photos supplied by Slabworks of Montana and Triton Stone.

Stroll through a retailer that sells paint, tile, stone, or anything else that comes in colors and flavors, and you’ll encounter an amusing selection of names for colorways. Customers face a staggering array of choices as they work through the details on new construction or remodels, and at times the decisions can feel paralyzing. Should your clients opt for Cloud White or Dune White for their trim color? Should the grout be Bleached Wood or Urban Putty?

As for the countertop, should they choose Mont Blanc, Mont Blanc, or perhaps Montblanc? Continuing the theme of copying natural stone, several quartz companies have usurped individual stone names and applied the exact same label to their manmade products. The original Mont Blanc is a genuine natural stone: a white quartzite with light grey layering. Mont Blanc is also the name of a slightly speckled pale grey manufactured product of one quartz producer. Montblanc is also a white and grey “marble-look” from a second quartz producer.

Some quartz product names intentionally evoke natural stone, such as this manufactured quartz offering called Calcutta Borghini (inset image), factory created and similarly named to compete with Calacatta Borghini marble, shown installed in this kitchen. Photos courtesy of Triton Stone.

This practice is widespread. Some quartz product names intentionally evoke natural stone: Capri Limestone, Charcoal Soapstone, Onyx Carrara, Calacatta Nuvo. Other cases are even bolder, taking the identical names from well-known stones and applying them to manmade versions. Super White, Taj Mahal, Emperador, Thassos, Nuage, and Statuario are all popular, prestigious natural stone, but they are also the names of synthetic countertops. How about Piatra Grey versus Pietra Grey? Do you know which one is real stone and which is an imposter?

I suspect that most in our industry can empathize with the potentially confusing choice designers and customers need to make. The best we can do is to help guide clients toward options that meet their needs, while providing education about different types of products. But when companies deliberately muddy the water and intentionally confuse their customers, it makes life harder for all of us.

Granite Comes From the Earth

Naming aside, what are the practical differences between manmade quartz products and genuine natural stone? Let’s start by looking at how each one is formed.

 A perpetually popular natural stone for countertops is granite, an igneous rock that was once molten magma. Magma occurs throughout the Earth’s crust: under volcanoes, along seams between tectonic plates, and in hotspots.

The texture of granite sheds light on its past. Magma that cools relatively quickly will have small and uniform crystals. Deep magmas cool more slowly. In the process they grow beautiful, large minerals with complex shapes that are evocative of their internal atomic geometry. Granites with super large minerals, called pegmatites, form when there is some water mixed with the magma, which spurs minerals to take shape more readily.

In all cases, the rock turns from liquid to solid over a span of thousands to millions of years, and takes shape miles deep within the Earth’s crust. These inexorably slow geologic processes forge a stone that is dense, durable, and will far outlast our lifetimes. Thanks to variations in the composition of the magma, granite comes in a span of all-natural colors, from nearly white, to coppery brown, to deep grey and black. Patterns range from mild to wild, with aesthetic variations to suit all styles and tastes. Each piece of natural stone is unique and each bears the mark of a particular time and place in our planet’s history.

Manmade Quartz Comes From a Mold

Manufactured quartz slabs are composed of three main ingredients: particles of mineral quartz, resins, and pigments. The quartz particles can vary in size from about 5 millimeters down to less than half a millimeter. Polyester resin binds the mineral pieces together. In some cases, the resin is mixed uniformly through the slab, and in other cases there are visible areas of resin, depending on the design. The same is true of pigments; some designs are the same color all the way through, while others have ribbons or accents of different hues, which are often meant to imitate the naturally occurring patterns in natural stone.

Manufactured quartz slabs are made by blending the ingredients, then pouring the mixture into a mold. Different manufacturers use different processes, but some combination of vibration, compaction, heat, and a vacuum are applied to cure the slabs from a slurry to a solid.

Testing the Hardness of Quartz Slabs

The website of a major quartz manufacturer makes this statement about the durability of its product:

  “[Company name] is much harder than granite or marble making it more durable. That means [company brand] is less likely to scratch, chip, or stain for years of worry-free service.”

Before we jump into a fact-check on hardness, it’s worth pausing to point out that hardness only relates to a surface’s resistance to being scratched. Hardness has little to do with chipping and nothing to do with staining.

Areas with pools of resin are often the softest part of a manufactured quartz surface. On this sample of Cambria Shirebrook, the resin is lightly scratched by a tool with a Mohs hardness of 6. Image courtesy of Karin Kirk.

 

Is quartz surfacing much harder than granite? This is straightforward to verify using metal picks calibrated to different hardness on Mohs scale. In test cases where the sample contained large particles of mineral quartz, the individual quartz grains yielded a hardness of 7. The “matrix” material around the larger particles were generally 6 to 7, with some areas between 5 and 6. Larger pools of resin were between 5 and 6. On colors where the particles are uniform and fine-grained, the hardness fell in the range of 6 to 7.

How does that compare to granite? Mineral quartz has a hardness of 7. Feldspar has a hardness of 6 to 6.5. These two minerals make up somewhere between 100% and 90% of a standard commercial granite. Other typical minerals in granite could include hornblende (hardness 5-6), pyroxene (hardness 5-6), biotite (hardness 2.5-3), and garnet (hardness 6.5-8.5).

I analyzed samples from several different quartz manufacturers. The Cambria samples I tested were similar to, or slightly softer than granite. Are they “much harder?” No.

This Caeasarstone sample is scratched by a metal tool that has a Mohs hardness of 6, and this result was repeated on several samples and colors. Therefore the hardness of these samples is less than 6. Caesarstone lists the hardness of their product as 6.5 to 7. Image courtesy of Karin Kirk.

Looking at other brands yielded similar findings. The fine-grained matrix on Caesarstone colors such as Buttermilk, Lagos Blue, and Pebble had a hardness of between 5 and 6, while larger, individual quartz particles in coarse-grained varieties were 7. Pental samples were largely between 6 and 7, with a few spots in the 5-6 range. LG Viatera samples came in right around 6 or slightly less. Silestone Nebula colors were also between 5 and 6.

These results make sense. Particles of quartz are a hardness of 7, regardless of whether they are in a natural stone or a manmade composite. Polyester filler and binder materials are softer than quartz, which is reflected in the softer values in those areas of the slab.

 “Dancing a Mighty Fine Line”

Fabricator Dave Scott has been making countertops for 25 years. He works in quartz, natural stone, and sintered ceramic materials and he appreciates the advantages of each. His shop, Slabworks of Montana, serves high-end clients near Big Sky and Yellowstone Club ski resorts, as well as more typical homeowners in the Bozeman area.

 “I’m not anti-quartz,” he explained, “but I’m just not a fan of some of their marketing.” In his experience, the biggest drawback of manufactured quartz is the way it can be damaged by heat. “I’ve replaced enough of them; I know,” he said wryly. Electric frying pans and slow cookers are some of the biggest culprits, he added, which can cause quartz surfaces to crack or scorch. Over the course of his career, Scott has seen numerous failures with cook top cutouts, more so than with natural stone slabs.

Scott noted that many quartz manufacturers list the upper end of the proportion of mineral quartz in their products, but they don’t often cite the lower ranges. “They range from the low 80s up to 93% at the top,” he said, while explaining that the solid colors typically have a lower percentage of quartz minerals.

When it comes to the way manufactured quartz companies call their products natural stone, Scott voiced some concerns. “Either you are [natural stone] or you’re not,” he quipped, adding that the claims of manmade quartz companies are “dancing a mighty fine line.”

“They’re trying to compare themselves to natural stone,” said Scott. He motioned out the window to the rows of granite, quartzite, and marble in the yard, adorned by recent snowfall, and continued emphatically, “But these are unique, God-made pieces of art for us to enjoy.”

And therein lies the essential difference between purely natural products versus engineered lookalikes. There can be no doubt that real stone is a product of the Earth, created by geology, God, or whichever combination you prefer.  Natural stones are natural, abundant, and fundamental parts of our planet. They bring life and energy into our homes and public spaces and are unquestionably authentic. Amid the confusion wrought by marketing strategies, perhaps the most useful conclusion lies in the age-old adage: Imitation is the sincerest form of flattery.

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A Scientific Guide to Shopping for Natural Stone https://usenaturalstone.org/scientific-guide-shopping-stone/ Fri, 08 Mar 2019 16:26:59 +0000 https://usenaturalstone.org/?p=5247 By experimenting on stone samples, you’ll not only gather key bits of information, but you’ll also gain confidence in the real-world attributes of various stones.

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A Scientific Guide to Shopping for Natural Stone

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Perusing slab yards is always an adventure. At first, it’s novel and exciting. Granite and marble and limestone, oh my! But aisle upon aisle of stone can trigger shopper’s overload. How can you tell them apart? Which one is right for you? Is Brazilian granite superior to Indian granite? And what to make of the enticing labels? Is Verde Butterfly Extra going to make your life better than Verde Butterfly Non-Extra?

Take a deep breath. We have answers for you. While subjective things like shades of off-white (ecru vs. cream?), stone names, and design trends can be dizzying, there is one tool that can reliably help you cut through the confusion. I’m talking about science, my friend.

Aside from the obvious fact that science is super cool and sexy, there’s a real advantage to this approach: you will learn for yourself how stones perform. By experimenting on stone samples, you’ll not only gather key bits of information, but you’ll also gain confidence in the real-world attributes of various stones. There’s nothing like your own personal experiences to reassure you that your stone is going to tick all the boxes for your situation.

 

Match the properties to the purpose

The first step is to assess your primary needs. A hardworking kitchen countertop in a family home might require durability as the top priority. A bathroom floor might favor texture and grip. A stone patio in Wisconsin needs to resist splitting, while the countertop at a bank will have to resist fingerprints and oils.

If possible, make a list of the properties that are most important to you before you head to the showrooms. That way, you can zero in on the types of stone that fit your criteria, and avoid the potential heartbreak of falling in love with slabs that don’t match your requirements.

 

Assemble your toolkit

We scientists love our gear, so here’s a list of items you can use to investigate stone samples:

  • Glass tile
  • Pocket knife
  • Small bottle of lemon juice or vinegar
  • Spray bottle of water
  • Cloth for wiping up water or acid
  • Magnifying glass (or use the magnifier function on your phone)
  • Camera and notebook to document your findings

 

Obtaining samples

As you evaluate various types of stone, be sure to explain to the sales staff that you’d like to do a little “sciencing” on some samples. Many dealers are happy to provide samples of stones that you’re considering. This is a smart practice because an educated customer is likely a satisfied customer. Fabrication shops are another source of potential samples, and the scrap bins offer a treasure trove of stones to satisfy your geologic curiosities.

Ideally, industry professionals will appreciate your desire to be as informed as possible, and can accommodate customers who want to ‘test drive’ stones before committing to a purchase. Who knows, perhaps salespeople will be similarly curious about a stone’s performance, and can help guide your investigations. In an age where information is passed along so easily, sometimes without regard for context or validity, it’s in everyone’s best interest to engage in our very own, science-based fact checking.

 

Hardness

In geology-speak, the hardness of a stone is its resistance to being scratched. Hardness is not the same thing as strength or durability, which we’ll get to in a moment.

Hardness is important when it comes to things like using metal utensils on your countertop, or scuffing muddy shoes across a stone floor. Of all the properties, hardness is the simplest to evaluate. Using a glass tile, check your stone sample to check to see if the stone scratches the glass.

A few tips:

  • Use a sharp corner of the stone.
  • Press hard, but be careful not to press so hard that you risk breaking the glass. Set the glass on a tabletop to do the test, rather than holding it in your hand.
  • There will almost always be a mark on the glass, but it’s not always an actual scratch. Wipe off any stone dust, then feel the scratch with your fingernail. Sometimes the stone simply ‘draws’ on the glass, and sometimes it scratches it. Get a little nerdy and investigate what’s really happening.

Another way to check the hardness of a stone is to use the tip of a knife blade to try to scratch the stone. One advantage of this method is you can examine individual minerals and check out different parts of the stone.

Stones that are harder than glass or a knife blade are likely to stand up well to wear and tear. Softer stones are still perfectly useful, even in high-wear areas, but it depends on your own preferences and needs.

 

Durability

How well a stone stands up to splitting, crumbling, and cracking are all part of its durability. This is harder to measure because it’s more subtle and subjective. Here are a few categories to investigate.

  • Splitting. Many types of stone are layered. Use a broken (not sawn) edge and see if you can peel apart the layers. How strong are the layers? This is especially useful for slate and schist, which have pronounced layering. The large “flashy” areas of layered mica can add stunning beauty to the overall appearance, but can flake off if near the surface.
  • Grains. All rocks are made of minerals, but in some cases those minerals are not stuck together too well. Investigate the edges of a stone and see if it’s possible to loosen or remove any grains. Use the tip of a pocketknife and have at it. In most cases, this test is a reassuring one. It’s not easy to pry grains out of a solid rock, and trying to do so will help you recognize the strength of your stone.
  • Cracks and fissures. A naturally occurring break in a stone slab is called a fissure, and if it’s human caused (during fabrication or handling, for example), then it’s considered a crack. Fissures in stone are a perfectly normal occurrence. All kinds of geologic stresses can cause a stone to fracture, and in many cases, these areas heal themselves with minerals carried along by groundwater. But once the stone is out of the ground, that process will no longer take place, of course. Weaknesses in the stone are mostly a concern during fabrication, transportation, and installation. Once the stone is in place, it’s not likely to break as long as it’s well supported underneath. That said, it’s wise to investigate any irregularities in a stone’s surface, regardless of if they are natural or not. Can you feel the edge of a fracture on the slab’s surface? If not, then the cracks/fissure is unlikely to be a problem. Does a fracture run all the way through the stone? Will it be near edges or overhangs? If so, then it’s a good idea to trim that area off the slab during fabrication.

 

Acid resistance

Acids can affect stones that contain calcite or dolomite: marble, dolomitic marble, limestone, travertine, or onyx. Acid sensitivity is another quality that can seem like a mystery, but is easy to measure. Use lemon juice or vinegar, puddle it on the stone, and let it sit for several minutes. Wipe off the acid, then look at the stone at a low angle. Etching looks like a dull area on the surface of the stone. When a stone etches, a tiny amount of the stone dissolves in the acid. This won’t affect the strength or longevity of the stone, but it does make a visual mark. Sealing does not prevent etching, but occasional re-polishing or re-honing will remove etch marks.

Some stones etch quickly and easily. Others take longer to show effects, and etch marks are less noticeable when they do occur. If you love marble but are concerned about etching, you can opt for a honed finish, which often makes etch marks less visible compared to a polished finish. Etching is less of a concern in areas where acids are not used, or for people who don’t aspire to perfection in their homes. So, acid reactions are not necessarily a deal breaker. But a little experimenting will tell you how your potential stone reacts, and will help guide your decision.

An important rule of thumb is that granite, quartzite, and soapstone do not contain acid sensitive minerals. If you want to be sure to avoid etching, then seek these types of stone and do the tests to be sure the stone is classified correctly.

One last clarification on this subject is that we’re talking about everyday acids like citrus, vinegar, wine, or tomato juice. Powerful acids like rust removers and toilet bowl cleaners are much more potent and should be kept away from all types of natural stone.

 

Staining/porosity

Everybody loves strawberries. But we don’t want to be perpetually reminded of them with a bright pink berry stain on the kitchen island. Staining is linked to porosity—in other words, how much open space exists within the solid matrix of the stone. Thankfully, the high pressures that bind rocks into solid forms tend to squeeze away most of the pore spaces. But different stones have been subjected to different amounts of squeezing, and thus, porosity varies among stone types.

Testing for porosity can be done a few different ways. You can put some water on the surface of an unsealed stone and watch what happens. Does it soak right in? If so, that’s a stone with high porosity. Does the water bead up, and wipe away cleanly? Then you’ve got a tightly compacted, low porosity stone on your hands. If the water doesn’t visibly soak in, but leaves behind a shadow or a damp spot when wiped away, then the stone has intermediate porosity.

If you want to get a little fancier, you can put stone pieces edge-wise in a shallow pan of water and see if water wicks up into the stone. Details about porosity tests are described in the Deep Dive Into the Properties of Quartzite.

You can also check for porosity using cooking oil, but bear in mind that oils will often leave a residue on the surface of the stone even if the oil doesn’t soak into the stone’s pores. After letting oil sit on the stone, scrub it with soapy water, rinse it, and then let it dry completely. At that point you can evaluate the oil’s effect on the stone.

Impregnating sealers should be used with porous stones, and a sealer will reduce or slow the rate of absorption to allow you to clean it before a stain becomes a problem. But that’s your second line of defense. Your best bet is to use the test to find a stone with a lower porosity in the first place, if that’s what your desired usage requires.

 

Why a basic granite satisfies most measures

There’s a reason why granite is such a popular type of natural stone. It scores well in all the diagnostic tests. It’s made of quartz and feldspar, which are harder than glass. It doesn’t split into layers, and the minerals are held tightly together in an interlocking, jigsaw-like arrangement. None of the minerals in granite are affected by everyday household acids. Granite is also beautiful, and thanks to the wonders of geology, comes in a stunning range of colors and patterns. It’s a win for its properties and its good looks.

It’s often said that knowledge is power—which is certainly applicable when it comes to gathering information and learning about any kind of big purchase. In the case of natural stone, you’ll not only learn about hardness, etching, and porosity, but you’ll also gain insights about geology and the planet. In the end, not only will that help you understand the traits of your natural stone, but it will help you appreciate its origins, too.

 

Basic supplies for a casual geology lab.
Testing the hardness of sandstone with a glass tile. The sandstone is harder than glass.
Testing the hardness of marble with the tip of a pocketknife. The marble is softer than the knife.
Ordinary white vinegar is useful for checking for acid sensitivity.
This soapstone has such low porosity that liquids puddle up on top of the stone surface, without soaking in at all.
Testing the porosity of sandstones and quartzites in a shallow pan of water for 15 minutes.
Testing the porosity of sandstones and quartzites in a shallow pan of water with pink food coloring.

 

SIMILAR ARTICLES:

soapstone geology durability of natural stone countertop comparisons chart

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Bookmatching: Geology Meets Geometry https://usenaturalstone.org/bookmatching/ Fri, 21 Dec 2018 08:00:10 +0000 https://usenaturalstone.org/?p=4800 Bookmatched slabs sometimes look like butterflies, or Rorschach (inkblot) tests, or many other fanciful shapes. Bar none, bookmatched slabs are one of the most dramatic and impressive ways to use natural stone.

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Bookmatching: Geology Meets Geometry

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You probably came here to read about marble, but for now, let’s talk about marble rye. The perfect medium for a salami, Swiss, and arugula sandwich. When it’s time to make a sandwich, I reach in the bag, grab two neighboring slices of bread, put them on a plate, and then flop them open like I’m opening a book. (A book about sandwiches, no doubt.)

Bookmatched Azul Imperiale.

The same idea – minus the salami – applies to marble stone slabs, as well. When two neighboring slabs are ‘opened up’ and polished on the surfaces that were facing each other, the pattern on each stone will be virtually identical, except they will be mirror images of each other. These twin slabs can then be arranged along a common edge to produce a stunning, kaleidoscopic pattern. Bookmatched slabs sometimes look like butterflies, or Rorschach (inkblot) tests, or many other fanciful shapes. Bar none, bookmatched slabs are one of the most dramatic and impressive ways to use natural stone.

Best places for bookmatching

A pair of bookmatched slabs commands a lot of attention. For maximum effect, these statement pieces should be used where there’s ample room to accommodate a large expanse of stone, like a big kitchen island, a conference room table, a wall, or an oversized shower. If you have a large area to cover, bookmatching is a handy way to ensure that the pattern runs fluidly from one piece to the next.

It’s not a great idea to cram a bookmatched pattern into a surface that’s interrupted by corners, cutouts, and appliances. The bigger the expanse, the greater the impact. That said, a bookmatched pattern need not be limited to full slabs. Smaller pieces of bookmatched stone are often used in flooring tile or backsplashes.

Variations on the bookmatch

Diamond matched marble wall. Photo courtesy of United Marble Fabricators.

If the standard two-slab bookmatch is somehow insufficient to satisfy your design tastes, you can take it up a notch with diamond-matching (also called quad-matching). This arrangement uses four pieces of stone, and is so named because it commonly produces a diamond-shaped pattern.

Bookmatched pieces needn’t be all on the same plane, either. A vertical slab on a wall can be mated to its twin on a horizontal countertop or bathtub surround, for example.  This gives an immersive effect, as if you are sitting inside of a vast block of stone.

Another variation on the theme is called vein-matching (or slip-matching), where the key visual elements of the slabs are matched to flow across seams and produce a continuous pattern. Vein-matching is commonly seen on ‘waterfall’ arrangements, where a horizontal countertop joins a vertical panel of stone that runs from the countertop down to the floor, or from the countertop up to the backsplash. Vein match in these instances is typically preferred over bookmatch.

Considerations when hunting for slabs

At the quarry, large blocks of stone are removed from the ground, then shipped to a facility for processing. Here, the big blocks are sliced into slabs. When the slabs are all polished on the same side, it’s called “consecutive” polishing (also called “sequential” polishing). These slabs are usually numbered so you can purchase neighboring slabs if needed.

To create a near-perfectly matched pattern, the surfaces of two neighboring slabs have to be processed so the surfaces that were facing each other are both polished. This operation is usually done when the slabs are cut from the block, and is not commonly done at a fabricator’s shop. In some cases it’s possible to convert sequential slabs to bookmatched slabs by polishing the back side of one of the slabs. But it’s less hassle and more reliable if the slabs were originally processed and polished with bookmatching in mind.

Because bookmatched slabs generally originate at the sawyer, there can be significant lead time if stone needs to be ordered. Plan ahead and be patient – the wait will be more that worth it.

Bookmatching tends to be more expensive than a standard layout, because in every case two slabs are needed, even if the area to be covered is not that large. And if one slab is lost to breakage or other issues, the entire layout of slabs can be lost due to the irreplaceability of the one slab. The painstaking planning and fabrication required to execute a precise match-up of the pieces may also add to the cost.

Any of the four edges of the slabs can be aligned. Showrooms often have bookmatched slabs on display like an open book, but keep in mind you can swap them left to right – or top to bottom – if you want. Each arrangement will yield a different pattern. You can mock up different variations to visualize the possible outcomes. The images below were created in PowerPoint by importing a single picture of a slab, copying it, making a mirror image of it, then dragging and rotating the two shapes to make different designs. For those who prefer a hands-on approach, you can print two photographs of the slab and fiddle with various layouts. (Warning: Regardless of the method, this is a mesmerizing and addictive process!)

While these graphics are electronically generated and show perfect mirror images, such perfection is not attainable in actual stone fabrication due to variation within the stone. Even in neighboring slabs, the patterns can vary over short distances, depending on the nature of the pattern and the direction of the grain. So, it is wise to expect a certain amount of non-uniformity amongst sibling slabs.

Since bookmatching requires two pieces of stone to be placed exactly next to each other, the edges of the slabs that are destined to be joined together have to be in near-perfect condition. Any chips, cracks, or awkward areas that are trimmed off of one of the slabs must also be removed from its mate.

Patterns: The good, the bad, and the whaaat?

Bookmatched Fusion granite.

The natural colors and patterns in stone will almost look amplified when presented in the mirror-image arrangement of a bookmatched pair. A certain amount of movement is required to create a visually interesting effect, but an overly complex stone can cause sensory overload. Stones with soft hues and flowing movement, like marble, will create a beautiful look that’s not too jarring. Vivid slabs with bright colors and high-contrast patterns are not for the faint of heart, but offer an unforgettable statement.

It’s practically inevitable that you’ll see images in the adjoining stones. Maybe it will look like a beautiful flower or a snowy owl. Or… maybe you’ll see the face of a malevolent goblin, or, heaven forbid, something resembling the, ummm, human anatomy? Once seen, these forms can’t be unseen; they will greet you every time you walk in the room. So take your time and carefully examine the potential designs and shapes you’ll end up with once the stones are cut and assembled.

Craftsmanship and communication

A downside to bookmatching is that there is little room for error in the fabrication and installation. The trimming and alignment of the slabs has to be spot-on. For this reason, careful communication with your fabricator is absolutely essential. Don’t assume you both know which way the slabs will be oriented and which parts will be cut off. Make sure that the fabricator has plenty of experience with bookmatched slabs, and that you share the exact same vision for the final product.

The best way to visualize and communicate the plans is with is with photographic images, mockups, and a dry-lay of the stone panels prior to installation. Many fabricators have the ability to import images of the slabs into computer software and then decide where each cut and seam will go. It’s imperative to go through this step together, and to sign off on the final plan. Neither the customer nor the fabricator wants any surprises on installation day, so if there was ever a time to be extra-careful in the planning phase, this is it.

Bookmatching is natural stone at its best

The coolest thing about bookmatching is that it takes the patterns of geology, which are plenty awesome on their own, and boosts them to an almost supernatural aesthetic. If you feel there’s no artist that can rival Mother Nature, then bookmatching might be for you. Pairing your own imagination with the inherent beauty of the Earth can forge a phenomenal result.

SIMILAR ARTICLES:

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Know Your Rocks: An Overview of the Geology of Natural Stone https://usenaturalstone.org/geology-natural-stone/ Wed, 21 Nov 2018 17:52:49 +0000 https://usenaturalstone.org/?p=4673 A bit of geology can shed light on why or where we’d want to use a given stone. Geology also helps us appreciate that every slab of stone offers a little glimpse into deep time and the dramatic forces that shape the planet.

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Know Your Rocks: An Overview of the Geology of Natural Stone

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Do you love natural stone? Me too. Fans of natural stone countertops, tiles, fireplaces, walls, and building stone are natural allies to geologists. We all share a similar zeal for a glimmer of garnet and the sexy sparkle of marble. The two disciplines have different ways of organizing and thinking about stone, which makes sense because we’re interested in different things. Geologists study rocks to learn more about what happened in Earth’s past. Regular people appreciate rocks because they’re useful, practical, and beautiful. Nonetheless, a bit of geology can shed light on why or where we’d want to use a given stone. Geology also helps us appreciate that every slab of stone offers a little glimpse into deep time and the dramatic forces that shape the planet.

This article touches on 13 different types of natural stone, with links to each type to explore further.

Organizing natural stones into categories

You learned this in 8th grade: Geologic categories of stone

Geologists, like all scientists, love to put things in categories. We group rocks by the process that formed them. Did a rock erupt from a fiery volcano, or take shape in a placid river bed?

Making more useful categories: Grouping stone by their properties

I’ll admit that geologic categories aren’t all that helpful for the way natural stones are used. Instead, we can group stones by the properties that matter to us, like how they hold up in the places we use them.

Here’s an overview of rock types sorted by hardness and their ability to withstand an onslaught of marinara sauce.

Note the empty category of hard stones that are damaged by acids. It turns out that hard minerals also tend to be unaffected by household acids. That’s just a coincidence of mineral chemistry, but it’s convenient for those looking for a hard, resistant natural surface.

When we talk about acid resistance, we’re referring to things like vinegar or citrus. Strong acids like oven cleaner and some bathroom cleaners will damage almost any stone, so keep those away from your stone, or better yet, use less toxic means to clean your home.

Relationships between different types of stone

In the world of geology, all stones are related to each other. Over deep spans of time, any rock can turn into a whole new rock if it gets melted, squeezed, uplifted, or eroded. In fact, that’s exactly what’s been happening all through Earth’s history. Understanding the relationships between different stones can make it easier to see why some share similar traits. It also helps you appreciate the events that gave rise to all those beautiful slabs in the showrooms.

Sedimentary rocks turn into metamorphic ones

Limestone forms in shallow, warm oceans and coral-rich beaches. It’s made of shells, shell fragments, and dissolved shells. Limestone can get buried and heated to taffy-like consistency, wherein it turns to marble. Both stones are made of the same mineral – calcite – but in marble’s case the calcite grains have been crystallized together, making the stone less porous. Marble’s distinctive grey streaks are clay layers from the original limestone that got heated and swirled.

The relationship between sandstone and quartzite follows a similar theme. Sand grains gather on beaches, sand dunes, and riverbanks. Layers of sand get buried and pressed together, forming sandstone. If sandstone gets shoved down deep and compressed even further, the sand grains fuse together to become quartzite. As described in the Deep Dive Into Quartzite article, this process is a gradual one. This means there are many gradations of sandstone and quartzite, ranging from highly porous sandstone to bombproof crystalline quartzite. The more deeply a stone is buried, the more tightly compacted it will get. The porosity of a stone translates into its ability to shrug off stains, and this is something that buyers can evaluate as they shop for different stones.

Bluestone is a variety of sandstone. It formed as rivers flowed off a former mountain range along the eastern seaboard. As 400,000,000 year-old rivers wound their way through the landscape, they left behind pockets of sandstone in Pennsylvania and southern New York. Because the sandy deposits occurred in small, scattered areas, the quarries were small, too, setting the stage for generations of family-run quarrying operations throughout the region.

Dialing up the heat on slate, schist, and gneiss

This trio of rocks shows what happens if you crank up the thermostat on a stone. The predecessor to all of these stones is shale, which is compressed clay and is decidedly un-sexy. But add a little heat and pressure and those unremarkable clay particles start to grow and strengthen and the rock turns into slate. Unlike shale, slate is durable – and is workable into tiles, shingles, and of course, old-school blackboards.

If the stone gets hotter, the clay particles morph into mica and the rock takes on a subtle sheen. This is called phyllite, but in commercial terms phyllite is usually sold as slate. More heat begets even larger mica grains, and the stone becomes schist, which is known for its glittery look. Schists with small mica grains are preferable to stones with large chunks of mica, because the latter can be weak and literally flaky.

Adding even more heat and pressure will make the stone separate into bands of light and dark minerals. Striped or banded patterns are the hallmark of gneiss. The patterns can be calm or bold, straight or swirled. For commercial purposes, gneiss is usually classified as granite, because it’s made of the same minerals, and shares similar properties and colors.

If the stone gets hotter still, it will start to melt. In some slabs of gneiss you can see melted blobs of quartz, showing the stone was right on the edge of becoming liquid again. If the whole thing melts, then you’ll end up with granite, an igneous rock.

The many colors of granite

Granite means many things. It’s a catch-all category that’s often used to describe any hard, crystalline stone. In geology, granite is one specific thing: an igneous rock that is coarse-grained and overall light-colored. But in the parlance of the natural stone industry, the definition of granite is expanded to include all igneous rocks, as well as many metamorphic rocks like gneiss and schist.

Geologists classify igneous rocks by the size of the crystals and the types of minerals. And while you will definitely sound smart if you casually inquire if your local slab yard has any quartz monzonite or granodiorite, that’s not necessary. Most igneous rocks are quite similar to each other, despite their different colors and patterns. We can just stick to calling them all granite. (Just please don’t tell my geology friends I said this!)

Basalt is one type of igneous rock that is famous for erupting out of volcanoes, like the spectacular lava flows from Kilauea we saw last spring and summer. Basalt also makes up the entire ocean crust (which itself is volcanic, betcha didn’t know that!) and forms oceanic islands like Hawaii and Iceland.

 

Solid rock from liquid water

Onyx and travertine are variations of the same stone. They come about from mineral-laden water, like you’d find at the mouth of a hot spring. Both are made of calcite, the same mineral that’s in limestone and marble. Travertine has a lacy pattern from the way the water flows in little rivulets away from the mouth of a hot spring. Onyx can form from either hot or cool water, and is less porous than travertine. Onyx is beloved for its smooth layers and gem-like colors that are especially glorious when backlit.

Last but not least: The oddball stone that doesn’t fit into any categories

It’s true with people and it’s true with stones, too. Not everyone fits into a tidy category. Soapstone, for instance, is basically nothing like other rocks. It manages to be soft, yet dense. You can scratch it with your fingernail, but you can’t stain it or burn it, no matter how careless you are. Soapstone is more like a family of stones rather than one specific thing, but it is cool stuff, and I bet it will surprise you.

Geologists and natural stone aficionados agree

Natural stone offers a lot to love—there’s zero doubt about that. Take a moment to learn about the history and characteristics of your favorite stone, and I bet you’ll appreciate it even more.

More from the Geology Series

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A Soft Spot for Soapstone https://usenaturalstone.org/soft-spot-soapstone/ Fri, 12 Oct 2018 21:52:07 +0000 https://usenaturalstone.org/?p=4505 Once you’ve come to terms with soapstone’s softness, you can revel in its strengths. Soapstone is remarkably resistant to staining or damage from acids. The density of the stone makes it practically impervious.

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A Soft Spot for Soapstone

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While browsing the slab yard or showroom, each type of stone seems to possess a distinct personality. Glossy, polished granite is the crisp tailored suit, while marble is like flowing linen—a little wrinkled but always in style. And soapstone? Without a doubt, it’s the flannel shirt of natural stone. Soft, touchable, and always comfortable. You can’t even walk by a slab of soapstone without stopping to pet it.

Soapstone enjoys a cult-like fan base: I love the organic-ness of it, writes one devotee on Houzz. But it’s not for everyone. I find these photos rather sobering, laments another commenter after viewing images of the patina that soapstone can acquire.

 

Yes, Soapstone is Soft

“All stones have benefits and disadvantages,” says Anthony Lacour of M. Teixeira. “There’s no such thing as a perfect surface.”

As the branch manager at M. Teixeira’s Denver office, Lacour has been working with this iconic stone for a dozen years. He suggests the best way to get a feel for soapstone’s hardness is to experience it personally. “Let people test for themselves,” he says.

Hardness of most commercial soapstones ranges from 1 to 4, but Lacour has found that the exact Mohs number is not as important as just getting a sense for it. “Use a fingernail and a key as your hardness indicators,” he advises.

Soapstone’s softness might be a dealbreaker for some—it comes down to knowing yourself and recognizing if a scratch in the stone is going to ruin your day, or how long it will take you to forgive a family member who accidentally drops a frying pan on the countertop.

Lacour explains the upside: “The good thing is that you can fix it yourself.”

A fresh coat of mineral oil will render small scratches invisible. Larger marks can be removed with sandpaper. Lacour recommends 120-220 grit for most scratches; if you prefer a shinier finish, you can follow up with 400-500 grit. Then re-oil the surface to restore the luster, and you’re all set.

Even a gouge is fixable—it can be filled with a mixture of stone chips and epoxy. This can be tackled by a professional or by a seasoned DIYer.

Steve Schrenk is the digital media director for Polycor, and he has worked with stone as a sculptor, fabricator, and designer. He describes soapstone as “very user friendly for self-repair,” noting that soapstone appeals to the type of person who “likes to roll up their sleeves and do it themselves.”

A Houzz commenter sums it up best, What I love love love the most about soapstone: If you are a DIYer at heart (or a control freak, like I am), then the self-maintenance of the counter is just wonderful.”

 

And Now for the Good News: Soapstone’s Superpowers

Once you’ve come to terms with soapstone’s softness, you can revel in its strengths. By and large, the stone is remarkably resistant to staining or damage from acids. The density of the stone makes it practically impervious. That smoldering casserole you left in the oven while binge-watching Better Call Saul? Put that right there on the stone, thank you very much.

These superpowers were not bestowed on soapstone by any magical process. It comes down to the properties of the minerals in soapstone. Soapstone’s primary ingredient, talc, is chemically inert, which is why soapstone is generally unaffected by acids and alkalines. Talc is also hydrophobic, meaning it quite literally repels water.

The mineral magnesite is another major component of soapstone, and it has the ability to retain heat. The properties of magnesite allow soapstone to work so well as an insulator or a fireplace. The stone is capable of absorbing heat and then slowly radiating it off, providing the long, sustained warmth so appreciated in cold climates. Lastly, soapstone is a dense arrangement of small minerals, with minimal pore space that might allow water to seep in. Low porosity means that soapstone will not absorb liquids nor harbor bacteria—a perk for the germaphobes among us.

Schrenk sums up the yin and yang of soapstone: “People tend to latch on to the scratching aspect of soapstone,” he says. But they may be “missing out on some of the other aspects of the stone” that make it so appealing.

 

Soapstone’s Quirky Geology

Soapstone is an unusual type of metamorphic rock. Most metamorphic rocks are heated and squished versions of their former selves. Limestone becomes marble. Sandstone turns to quartzite. But soapstone doesn’t abide that simple recipe. Soapstone comes about from a series of chemical reactions that take place deep underground. Hot groundwater carries dissolved minerals from one rock to another, allowing a mingling of ingredients that begets entirely new minerals. In some cases, soapstone is a derivative of dolomite or dolomitic marble (like Super White). In others, soapstone comes from ultra-deep, ultra-dense rocks from Earth’s mantle. In this latter case, serpentine is also formed, and hence, soapstone and serpentine can often be found side-by-side in a quarry or outcrop.

Soapstone’s signature soapiness comes from the mineral talc. Talc is a member of the mica family, and is made up of thin flakes. The flakes are held together by a very weak type of bond, which allows the layers to easily slide against each other, giving the stone a slippery feel.

Talc is the softest mineral on Earth, with a hardness value of 1. Soapstone always contains some talc, but the amount varies, and therefore so does the overall hardness of soapstone. Stones with high talc content are called steatite, and are useful for carving. Commercial soapstone slabs generally have 30% to 50% talc, with the remainder of the stone being chlorite, magnesite, amphibole, and other minerals. In general, the lower the talc content, the greater the hardness.

Geologically, soapstone is a family of stones rather than one specific thing. There’s broad variation in the types of minerals present and their proportions. This is all the more reason to thoroughly investigate potential stones and to work with reputable dealers and fabricators.

If a stone looks sort of like soapstone but can’t be easily scratched with a pocketknife, it’s likely serpentine rather than soapstone. Virginia Mist and Jet Mist are granites that resemble soapstones, but are much harder. When in doubt, use the diagram below and read up on how to tell green stones apart.

 

Evaluating the Hardness of Various Soapstones

Soapstone really is different from most other types of stone. What better way to explore this than to try a battery of tests and see how it performs. M. Teixeira sells a sample kit of various soapstones to allow customers to experience a range of soapstone colors, textures, and hardnesses. I used a set of Mohs hardness picks to get up close and personal with the hardness of 12 soapstones. I tried to scratch different minerals in the stone with picks of various hardness values. I also used my fingernail and a pocketknife so that I could compare common items with Mohs numbers.

The results varied depending on how much talc the stone contained and what other minerals were present. While all the samples fell into a range between 1 and 4, they were different from one another, and even a single stone could have different hardness values in different places.

A summary of soapstone hardness is given in the table below, and the stones are arranged roughly from softer to harder.

 

Testing Acid Resistance

After I checked out the hardness of the 12 soapstones, I moved on to acid tests. I put a 10% solution of hydrochloric acid on every sample, and also used standard white vinegar to check for etching. I left the acids there for at least a half hour, before scrubbing the stones with soap and water and inspecting them for damage.

Several stones had a slight bubbling reaction with hydrochloric acid. This is expected because soapstone sometimes has calcite veins, and/or it can contain magnesite, which will have a very subtle reaction to acid. Interestingly though, 11 of the 12 stones showed no damage, etching, or staining from the hydrochloric acid, even though the acid initially looked like it had stained some of the stones. But it washed away and left the stone unaffected. Similarly, vinegar left no mark whatsoever on 11 of the 12 stones.

One stone, Stormy Black, showed a faint etch mark where vinegar was left puddled up for several hours, and the hydrochloric acid left a stippled white pattern on the black stone when left for an hour. This stone appears to be somewhat susceptible to acids, and likely has more magnesite than the other samples. The dark color and fine texture of Stormy Black may also make the changes appear more noticeable.

Aside from that, the other 11 samples looked brand “new” (while appreciating the fact that they are indeed several million years old!).

 

Oiling or Waxing Enhances the Finish of Soapstone

Soapstone can have two distinct looks, depending on the finish. It can be left untreated and will attain a soft grey color and a matte finish. Or, the surface can be oiled or waxed, which will darken the color and impart a satiny luster. “You get multiple looks from the same stone,” says Lacour.

To oil, or not to oil: that is a frequent dilemma among soapstone owners. Light oil like mineral oil is easy to wipe on but will fade fairly quickly. Wax can also be used as a surface treatment. It requires more effort to apply, but it lasts longer. An oil/wax blend strikes a happy medium between the two.

One needn’t agonize over this decision, because it’s always reversible. Thanks to soapstone’s density, the oil simply sits on the surface. It doesn’t penetrate the stone. If you change your mind and decide you don’t like the oiled look of your soapstone, you can scrub most of it off right away, or simply wait for it to disappear on its own.

One minor caveat to the oiled vs. naked finish is the color of the seams. During installation, the epoxy in the seams will be dyed to match the stone. But since the color of the stone depends on whether it’s oiled or not, you could end up with a slight mismatch. When in doubt, savvy soapstone owners suggest going with a lighter color in the seams, because the seam can be darkened more easily than it can be made lighter.

 

Best Uses for Soapstone

Around the world, soapstone has been shaped into cooking pots, utensils, vessels, and sculptures for thousands of years. Soapstone’s workability made it especially useful during the Bronze Age, when molds were carved out of soapstone and filled with molten metal.

Today, soapstone is a beloved material for wood stoves and fireplaces. At the Bridger Bowl ski area in frigid Montana, a soapstone stove is the central feature in a slopeside warming hut. The stove is thoughtfully placed in the middle of the room, beckoning to visitors and easing the woes of chilly children. Once heated, the stone gives off warmth long after the fire goes out. Even after sitting idle all night long, the soapstone is still warm the next morning.

Soapstone is well known as a worktop in laboratories, where its chemical inertness and heat resistance allow it to withstand all manner of abuses.

These same traits make soapstone an enviable material in the kitchen, where it’s commonly used for countertops, islands, or sinks. Unlike many types of natural stone, soapstone cannot be polished to a glossy shine. Instead, it has a soft, warm glow and rounded edges that help a space feel comfortable rather than imposing. Our kitchen looks loved! It looks lived in! People who eat together and tell stories and make each other laugh and spill their drinks live here!” writes a fan of soapstone on Houzz.

Both Lacour and Schrenk agree that soapstone fills a distinct niche in the industry. Soapstone’s grey tones and honed finish are on-trend nowadays, but soapstone won’t ever go out of style. While some stones draw attention to themselves, “soapstone’s subtle colors plays well with other elements of design,” explains Schrenk. “It fits a 100 year old building or new construction,” observes Lacour. Schrenk echoes the same sentiment: “It’s modern use of a traditional material.”

 

Alberene – Virginia’s Soapstone Quarry

Not far from Charlottesville, Virginia sits a large soapstone deposit and an active quarry that dates back to 1883. Over the years, Alberene soapstone was destined for a variety of applications, ranging from industrial uses of talc in tires and roof shingles, to practical objects like sinks, bed warmers, and griddles. Polycor purchased the Alberene quarry 5 years ago, and they’ve been pleasantly surprised by the enduring popularity of soapstone. “It’s surpassed everyone’s expectations,” says Schrenk. Alberene’s most popular soapstone is called Church Hill, literally named because of a hilltop church near the quarry. Nowadays, the quarry mostly produces slabs destined to become countertops, tiles, pavers, treads, wall caps, and fireplace inserts. “There’s a huge surge right now, especially for countertops,” says Schrenk.

The uptick in demand is easy to appreciate. Alberene soapstone is local, natural, and has “a tactile quality” that customers are drawn to, explains Schrenk. He finds that once customers learn what sets soapstone apart from other stones, “they sing its praises.”

 

Is Soapstone Right for You?

Choosing stone is always a personal decision, but even more so with soapstone. Only you know your situation and squeamishness, and Lacour’s advice to test the stone yourself rings true. Thankfully, soapstone dealers typically provide samples for customers to work with, so you can bring pieces home and try out your own scratching, etching, and staining tests. (You can also take our Stone Personality quiz.)

This bit of online advice nails it: “I’m looking forward to the aging and patina. But it would be sad if someone who wasn’t up for it spent a lot of money and had their heart broken.”

As with every material, the more you learn about it and the better you understand your own needs, the easier it will be to narrow down your choices.

If you’re curious about soapstone, spend some time interacting with it and see what you think. I found myself falling more in love with the samples the more I played with them. Another Houzz commenter said it best: “To those of you considering soapstone, do not be afraid!”

 

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