Gemologist Guide to Identifying Epidote

Epidote is a fairly common mineral that is collected by crystal and mineral enthusiasts. This incredible mineral forms elongated crystals that are often interconnected and lustrous. The interesting thing about this mineral is that it can be found as an inclusion in crystals as well as a standalone crystal cluster.

 

How to Identify Epidote Through Testing

There are various ways to identify rocks, minerals, crystals, and gemstones, but we will use a method I learned while attending the Gemological Institute of America.  If you’ve learned a unique way to identify gems, please share it with us.

Let’s look deeper into how to identify Epidote like a pro. 

 

 

Visual Inspection

The visual inspection starts with what form of Epidote you have.  The questions below are relatively easy to answer, but each type will have its own process for identifying them.

 

 

Is it a cabochon? From time to time you will see Epidote cut into a cabochon but it is not common. If you do come across a cab then it will have a medium polish and you’ll see pitting on the surface. It also has a tendency to be brittle. 

 

 

Is it faceted? If you have a faceted piece of Epidote, it should be opaque. Try shining a light through it; you shouldn’t see transparency in the stone. It’s pretty rare to find a faceted piece of Epidote and I wouldn’t expect you to see this while looking at stones.

 

 

Is it a specimen? Epidote is found in different forms. You’ll get better at identifying these forms by looking at and inspecting this mineral over time. Here’s a list of characteristics Epidote displays when it’s a specimen.

• Epidote crystals typically grow in elongated forms.
• Crystals have a strong pleochroism.
• Specimens have a brittle tenacity.

 

Is it tumbled? While Epidote can be found tumbled, it doesn’t take a good polish like many other stones do, which can make them slightly fragile. They’re best for display instead of carrying around in a pocket.

 

 

Physical Properties of Epidote

Let’s take a look at the physical properties of Epidote. Knowing what to look for will help you more easily identify what you’re looking at.

 

Color: Yellow-Green, Green, Brownish-Green, Blackish-Green, Black

Clarity / Transparency: Transparent, Translucent, Opaque

Luster: Vitreous

Cleavage: Perfect on {001} Imperfect on {100}

Fracture: Irregular/Uneven

 

The Streak Test

This is a destructive test, so you must ensure that you can damage the specimen or stone if you choose to use this method.  You won’t use destructive tests once you’ve developed robust knowledge in identifying rocks and minerals.

A mineral streak test is when you scrape the stone against a harder surface to see what color remains. Epidote’s streak is colorless.

Tumbled specimens are tested by scraping samples across a piece of ungalvanized porcelain, typically known as a streak plate.

 

Magnet Test

Epidote is slightly magnetic due to its ferrous oxide content. However, none of the other materials within the gems are.

 

Epidote Hardness Test

I don’t recommend actively testing the hardness of a stone because it’s destructive in nature and doesn’t really provide a definite answer to what type of stone it is.  Epidote has a hardness of 6 on the Mohs hardness scale.

 

Refractive Index Test

Determining the refractive index, or RI, as it’s referred to by gemologists for Epidote, is relatively straightforward. Still, you’ll need a specific piece of test equipment and the RI fluid to go with it.  Before you place the stone on the refractometer, you want to make sure you have a flat, somewhat polished surface to take a reading.

 

Epidote’s Refractive Index: 1.715 – 1.797

 

Each gemstone has its own RI, so discovering a sample’s RI can help you figure out what sort of stone it actually is.

 

Step 1 – Place a small bead of RI fluid on the metal surface of the refractometer near the back of the crystal hemicylinder (the window on which the stone will sit).

Step 2 – Place the stone facet face down on the fluid dot and slide it toward the middle of the hemicylinder crystal using your fingers.

Step 3 – Look through the viewer lens without magnification. Continue looking until you see the outline of a bubble, then look at the bottom of this bubble. Take the reading from there, rounding the decimal to the nearest hundredth.

 

Occasionally, you’ll run into the issue of not having a flat surface to work with.  In this instance, you’ll need to leave the top of the refractometer open and hold the rounded stone with your hand.  Hopefully, you can pull a reading off of the gauge.

 

Birefringence Test

Consider testing the birefringence, as well. Birefringence is related to RI. While doing the birefringence test, you will turn the gemstone on the refractometer six times throughout the observation period and note the changes.

Perform a standard RI test. Instead of keeping the stone still, gradually turn it 180 degrees, making each separate turn about 30 degrees. At each 30-degree mark, take a new RI reading.

Subtract the lowest reading from the highest to find the stone’s birefringence. Round it to the nearest thousandth.

 

Birefringence: 0.019 – 0.046

 

Single or Double Refraction

Epidote displays an incredibly low double refraction.

The stone must be transparent for this test to be accurate and beneficial.  If the light won’t pass through the stone, there is no way to test for single or double refraction.

Check for single or double refraction. Use this test on translucent and transparent stones. You can determine whether the stone is only singly refractive (SR) or doubly refractive (DR) to help identify it. Some stones can also be classified as aggregate (AGG).

Turn on the light of a polariscope and place the stone face down on the lower glass lens (polarizer). Look through the top lens (analyzer), turning the top lens until the area around the stone looks darkest. This is your starting point.

Turn the analyzer 360 degrees and watch how the light around the stone changes.

If the stone appears dark and stays dark, it is likely an SR. If the stone starts out light and remains light, it is likely AGG. If the lightness or darkness of the stone changes, it is likely DR.

 

Checking The Diaphaneity

Diaphaneity refers to the mineral’s ability to transmit light. For instance, some minerals are transparent or translucent. A small amount of distortion might occur when they’re thick, but light will pass through them relatively freely.

Epidote is transparent to translucent to opaque.

 

Finding The Specific Gravity

Every stone has its unique specific gravity, which helps us identify them. Specific gravity is one of the best properties to measure when identifying mineral specimens. Most minerals have a narrow range of specific gravity, so getting an accurate measurement can go a long way toward identification.

Specific gravity is a unitless number describing how heavy a mineral is compared to equal volumes of water. For example, if a mineral is three times as dense as water, it’ll have a specific gravity of three. This is useful because while two minerals might be the same size, they’ll each have a different specific gravity.

The larger the sample, the more precise the readings tend to be. Remember that this technique can only be used for single mineral or crystal masses. It will not work for minerals embedded in host rocks.

 

Epidote’s Specific Gravity: 3.38 – 3.49

 

As helpful as specific gravity is for identifying minerals, amateurs are usually constrained by the need for more necessary tools for the job. However, one way to work around this is to hold the specimen and note how heavy or heft it feels compared to what you might expect a specimen of that size to weigh.

If you want to determine the specific gravity of your stone like a pro, you’ll need to invest in a higher-end scale.  The OHAUS Density Determination Kit is the one gemologists use.

 

Identifying Rocks and Minerals Like a Pro

Hopefully, you feel confident in your practice of identifying a piece of Epidote after reading and applying this guide.  You’ll be using the visual part of this guide the most, and you’ll get better as you interact with more gemstones.  Before you know it, you’ll be identifying stones like a gemologist.

Feel free to reach out if you encounter any issues or need clarification. I’ll do my best to assist you in the identification process.