Finding peridot in Washington takes some knowledge, but the right locations can lead to exciting discoveries. A few areas have produced this gemstone, and knowing where to search improves your chances.

The right combination of minerals and conditions has allowed peridot to form in certain parts of the state. If you know what to look for, you might spot pieces hidden among the rocks.

We’ll help you find the best places in Washington where peridot has been found. With the right approach, you’ll have a better chance of adding this gemstone to your collection.

How Peridot Forms Here

Peridot forms deep within Earth’s mantle, around 20 to 55 miles below the surface, where intense heat and pressure create the perfect conditions. It’s actually made from magma that cools super slowly, letting the crystals grow nice and big.

The main ingredient is olivine, which needs temperatures between 1,000°C to 1,300°C to form properly. When volcanoes erupt, they sometimes bring these green gems up with them in basalt rocks.

What’s really cool is that peridot can also come from meteorites – yep, some of these crystals literally fell from space! The iron and magnesium inside the stone is what gives it that signature olive-green color.

Types of Peridot

Peridot’s value fluctuates based on its origin and quality, with its vivid colors making it a distinctive and sought-after gemstone. Here are the different types of Peridot:

Burmese Peridot

Burmese Peridot shows off a pure, bright green color that looks almost like spring leaves. Most other peridots have brown or yellow mixed in, but Burmese ones usually don’t.

The stone’s special green color comes from the iron inside the crystal. When light hits it, the stone seems to glow from within, creating a beautiful effect that catches everyone’s eye.

These stones often have special markings inside called “lily pads.” These are small, round patterns that look like tiny circles when you look at them with a magnifying glass.

You can often find Burmese Peridot in larger sizes, which makes them great for bigger jewelry pieces. The stones keep their bright color even under different kinds of lighting, so they look good both in sunlight and indoor light.

Pakistani Peridot

Pakistani Peridot is known for its vibrant green hues, which can range from yellow-green to olive green. The stones are usually very clear and shine beautifully when light hits them.

The stone typically has a vitreous luster and can be quite transparent, showcasing its brilliance. High-quality specimens can exhibit exceptional clarity with minimal inclusions, which enhances their appeal in jewelry.

Inside these stones, you might find tiny bubbles of liquid and gas. These create interesting patterns that make each stone has its unique pattern of these markings.

These peridots often come in larger sizes and maintain their bright color even under artificial light. This makes them look just as good in the evening as they do during the day, which is why some people call them “evening emeralds.”

Arizona Peridot

Arizona Peridot shows off a bright, lime-green color that sometimes has olive tones. The stones are usually smaller than other peridots but make up for it with their exceptional brightness and sparkle.

These stones often have a special kind of clarity that makes them appear very clean to the naked eye. When you look at them closely, you might see tiny specks of black minerals inside, which are typical of Arizona stones.

Arizona Peridot is especially famous due to its association with the San Carlos Apache Reservation, which is one of the largest sources of peridot in the world. The region’s peridot is highly valued not only locally but also within the broader gemstone market for its quality and vibrant color.

Changbai Peridot

Changbai Peridot displays a deep, rich green color that sets it apart. Their color is more intense than other peridots, showing deep forest green tones.

These stones usually come in medium sizes, around one carat. What makes them special is how clean they look – most have very few internal marks or inclusions. This clarity lets more light pass through, making them especially bright and sparkly.

The color of Changbai Peridot stays consistent throughout the stone. Unlike some other peridots that might show patches of different colors, these maintain their rich green tone evenly. This makes them particularly appealing when set in jewelry.

Their superior clarity and rich color have made them increasingly popular since 2005. Even though they’re newer to the market compared to other peridots, they’ve quickly gained recognition for their outstanding quality.

Vietnam Peridot

Vietnam Peridot, also known as chrysolite, has a special yellowish-green color that makes it easy to spot. They often come in larger sizes than peridots from other places.

When light passes through these stones, it creates a unique double-image effect. If you look closely at a faceted stone, you might see the edges appear doubled. This effect makes them sparkle in a special way.

Vietnamese peridot is often found in mafic and ultramafic rocks, which are rich in iron and magnesium, leading to the formation of larger and higher-quality stones.

The green color stays even throughout the whole stone. This consistent color is one reason why collectors really like Vietnam Peridot.

Norway Peridot

Norway Peridot comes in beautiful olive green shades. The color can range from light yellow-green to deep olive. The amount of iron inside the stone decides how dark or light the green will be.

When light enters these stones, it splits into two beams. This makes the stone look extra sparkly and bright, even when the light isn’t very strong. You can see this special effect best in well-cut stones.

Norway Peridot is part of a long tradition of peridot use in jewelry and artifacts, including significant pieces like those found in the Shrine of the Three Kings in Cologne Cathedral, which were initially thought to be emeralds but were later identified as large peridots.

Pallasite Peridot

Pallasite Peridot comes from space! These green crystals are found inside meteorites, mixed with metal from space. The green crystals stand out beautifully against the silvery-gray metal background.

These stones form a natural pattern in the meteorite. The mix of bright green crystals and shiny metal creates a beautiful design that looks like stained glass when light shines through it.

Scientists find these stones especially interesting because they tell us about how planets form. The mix of metal and crystal shows us what the inside of planets might look like.

These stones are pretty rare since they only come from meteorites. Collectors really like them because each piece tells a story about space and has its own unique pattern of green crystals.

Antarctica Peridot

Antarctica Peridot usually comes in smaller sizes, but each stone packs a lot of sparkle. They show a pure green color that can look slightly yellowish or olive in different lights.

These stones formed under extreme cold conditions, which affects how they look. They tend to be very clear with few internal markings. Most pieces are under two carats in size.

The extreme conditions where these stones formed make them special. They had to survive intense pressure and cold temperatures to reach the surface.

These stones are among the rarest peridots because they’re so hard to find. Their small size actually helps them sparkle more intensely than larger stones.

Hawaii Peridot

Hawaii Peridot has a rich olive-green color. Inside many stones, you can find special bubble-shaped marks called “lily pads.” These marks look like tiny round discs frozen in the stone.

One cool thing about these stones is that some of them contain tiny bits of gas trapped inside from when they formed. Scientists can study these bubbles to learn about conditions deep in the Earth.

In Hawaiian culture, peridot is associated with Pele, the goddess of fire and volcanoes, which adds to its allure among collectors interested in cultural artifacts.

New Mexico Peridot

New Mexico peridot typically ranges in color from brown and greenish-brown to yellowish-green and the more desirable green hue. This variety stands out due to its potential for a wider color range compared to peridot from other regions.

One notable aspect of New Mexico peridot is its occurrence in volcanic debris from ancient eruptions, specifically from a 180,000-year-old volcano. This geological background contributes to the unique properties of the stones found there.

The Kilbourne Hole area is particularly noted for producing high-quality peridot that is sometimes considered superior to that from Arizona.

What Rough Peridot Looks Like

Peridot has several distinctive characteristics that can help you identify it in its natural form. These are the key features to look for.

You also want to make sure you know what else you’re looking at. Many rockhounds don’t really know what they’re finding and tossing away.

DON'T MISS OUT ON ANY GREAT FINDS!

While you're out searching for Peridot you're going to find A LOT of other interesting rocks and minerals along the way. The last thing you want to do is toss out something really interesting or valuable. It can be easy to misidentify things without a little guidance.

You absolutely need a good reference guide in order to understand what you're looking at!

We've put together a fantastic field guide that makes identifying 140 of the most interesting and valuable rocks and minerals you will find REALLY EASY. It's simple to use, really durable, and will allow you to identify just about any rock and mineral you come across. Make sure you bring it along on your hunt!

Now, back to the identification specifics:

Check for a glassy or waxy luster

Raw peridot typically shows a distinct glassy to waxy shine, even in its unpolished state. When you shine a light on it, you’ll notice it’s not quite as sparkly as quartz but definitely shinier than most common rocks.

Pro tip: if it looks kind of like olive oil frozen in stone form, you might be onto something!

Look for that signature olive-green color

Unlike other green stones, peridot has this unique yellowish-green to olive-green color that’s pretty consistent throughout the stone.

Here’s the thing – even when rough, it shouldn’t have dark spots or zones. If you spot patches of brown or black, you’re probably looking at something else.

Hold it up to natural light – a genuine peridot will show that characteristic color even in its rough form.

Examine the crystal structure

In its natural state, peridot forms stubby, prismatic crystals. Look for somewhat rectangular or barrel-shaped formations – they might be rough, but you should see hints of this shape.

Sometimes you’ll spot these crystals embedded in darker volcanic rock (that’s basalt, by the way). The surfaces might look a bit pitted or weathered, but they shouldn’t be perfectly smooth.

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Tips on Where to Look

Peridot typically forms in volcanic areas and can be found in several accessible locations. Here’s where you should start looking:

Volcanic Rock Formations

Look for dark-colored basalt rocks and olivine-rich formations. Check areas where ancient lava flows have created large rock deposits, especially those with visible green crystals embedded in the rock. These rocks often weather over time, exposing the peridot crystals.

Stream Beds and Gravel Banks

Search in stream beds where water has naturally broken down volcanic rocks. Peridot is usually more concentrated in these areas because water carries away lighter materials while leaving behind heavier minerals.

This makes it easier to spot the olive-green crystals among the gravels and sands that have accumulated over time.

Old Mining Areas

Visit abandoned mine dumps and tailings, particularly those known for copper or nickel mining operations that were active in volcanic regions.

These areas often contain peridot as a secondary mineral, and since the rock has already been broken down during previous mining operations, the gems are easier to spot.

The types of Peridot you can find around the state

In Washington, peridot comes in vibrant green colors, with some stones showing hints of olive or yellow. The most common types are similar to those found in places like Arizona and Pakistan, displaying bright lime-green shades.

These peridots are often small but valued for their clarity and sparkle. They shine with a vitreous luster, especially when exposed to light in volcanic rock areas.

Some Great Places To Start

Here are some of the better places in the state to start looking for peridot:

Snoqualmie River area

The Snoqualmie River runs through areas where peridot could be present, carried downstream from sources higher in the mountains. Gravel bars and rocky outcrops along the river may hold small pieces mixed with other minerals.

Upstream channels and tributaries can bring materials from deep underground, depositing them where the water slows. Areas with exposed bedrock or fresh erosion might be good places to check, especially after heavy rainfall.

Seasonal changes and strong currents can shift sediments, revealing new finds along the riverbanks. Searching when the sun is bright can help, as peridot’s color stands out more when wet.

Ellensburg

Ellensburg has a rugged landscape shaped by volcanic activity, creating a mix of rock formations that attract collectors. The area’s basalt flows are a potential source for the green gemstone.

Older lava flows and exposed rocky outcrops offer good spots to search, as erosion can reveal fresh material. Dry streambeds and gravel deposits are also worth checking, as water movement can concentrate loose stones in one place.

With its mix of volcanic rock and shifting waterways, Ellensburg provides conditions where peridot can be found. Searching the right locations could uncover pieces of this bright green mineral hidden among the region’s diverse geology.

Columbia River

The Columbia River has carved through thick layers of volcanic rock, exposing formations that contain a variety of minerals. Olivine, the mineral that forms peridot, is found in some of the basalt flows in the area.

Erosion has helped uncover sections of these formations, creating opportunities to find peridot. Searching areas with exposed basalt and rocky outcrops could lead to discoveries of this gemstone.

Gravel deposits and dry streambeds near the river are also worth exploring, as water can transport and concentrate loose stones. With the right conditions, peridot can be found where these geological processes have revealed fresh material.

Skagit River

The Skagit River flows through the North Cascades, cutting through rugged terrain where various minerals can be found. Some sections of the riverbed and nearby gravel bars contain olivine-rich rocks, which could include peridot in certain areas.

Upstream sections, where the river runs through igneous formations, are more promising for mineral hunters. The shifting waters expose new material over time, making some gravel deposits worth investigating.

Tributaries feeding into the river also carry material from surrounding mountains, adding to the variety of rocks along the banks. Searching after seasonal floods may reveal fresh deposits that were previously buried.

Blue Mountains

The Blue Mountains rise over southeastern Washington, shaped by volcanic forces that left behind thick basalt formations. Some of these formations contain peridot, which can be found where erosion has exposed fresh material.

Rocky slopes and weathered outcrops provide good spots to search for this green gemstone. Dry washes and gravel deposits are also worth exploring, as water can transport and concentrate loose stones.

Peridot may turn up in areas where natural forces have broken down the surrounding rock. Streambeds and eroded hillsides offer promising locations to look for pieces that have been freed from the basalt.

Places Peridot has been found by County

After discussing our top picks, we wanted to discuss the other places on our list. Below is a list of the additional locations where we have succeeded, along with a breakdown of each place by county.