Colorado’s amazing geology isn’t just about those famous Rocky Mountains. Our state sits on some of the richest mineral deposits in the country, including beautiful olive-green peridot crystals.

Many rockhounds waste countless hours searching in the wrong spots, only to go home empty-handed. We know how frustrating that can be – we’ve been there too.

After years of exploring Colorado’s peridot spots and talking to local collectors, we’ve put together a list of proven locations where you’re most likely to find these gems.

These aren’t just random spots from the internet – we’ve visited each one ourselves and even included some lesser-known areas that tourists often miss.

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 Look Like?

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

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.

A Quick Request About Collecting

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.

Some Great Places To Start

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

Buena Vista

Buena Vista is located right by the Arkansas River in Colorado. The town has mountains on both sides – the Sawatch Range to the west and the Mosquito Range to the east. This special spot at the meeting point of different rock types makes it great for finding gemstones.

The area is famous for its “fourteen-ers” – mountains that are over 14,000 feet tall. These mountains and the river valley create perfect conditions for finding gems.

Peridot hunters often look in the stream beds where the Arkansas River has washed down minerals from the mountains. The best spots are usually where you can see bare rock sticking out of the ground.

The green peridot found here often shows up in places where different types of rock meet. Rockhounds can explore the public lands around town, especially areas where mountain streams meet the main river.

Salida

Salida sits in Chaffee County, Colorado, where the Arkansas River flows through the southern Mosquito Range. The town is a gateway to the Rocky Mountains and draws both outdoor enthusiasts and rock collectors.

Here, you’ll find ancient metamorphic rocks that formed deep underground, plus younger volcanic rocks from old eruptions. This mix of different rock types makes Salida special for finding minerals.

The mountains around Salida contain various gemstones and minerals thanks to its rich geological past.

Peridot hunters can explore the volcanic rocks near town, particularly in the surrounding foothills. The best spots are often where dark-colored igneous rocks are exposed.

Hartsel

Hartsel is a small town in central Colorado, sitting in the wide South Park basin of the Rocky Mountains. The town’s location at 8,900 feet above sea level makes it a unique spot for rock collectors and nature lovers.

The ground here has a mix of very old rocks from the Proterozoic period and newer sediments. This mix creates good conditions for finding different types of minerals.

The best places to look for peridot are near old volcanic areas around town. Check the gravel beds and small streams that flow down from the mountains. These streams often carry minerals from higher ground.

The dirt roads leading away from town can also be good spots to search, as rain and wind expose new rocks.

Mount Antero

Mount Antero is a tall mountain peak in Colorado’s Rocky Mountains, about 12 miles from the town of Buena Vista. The mountain sits in San Isabel National Forest and is known as one of the highest gem-collecting spots in the world.

The mountain is famous for its rich deposits of beautiful gems and minerals. Its granite rocks have special holes and pockets called miarolitic cavities that hold various crystals.

The best way to look for peridot is to search the granite areas along Mount Antero Road. The saddle area between Mount Antero and Mount White is a good spot to start.

The higher areas of the mountain, above 12,000 feet, have produced some of the best mineral specimens. Remember that the weather can change quickly at these high spots, so plan your visit during the summer months.

Arkansas River

The Arkansas River runs through Chaffee County in central Colorado, right in the heart of the Rocky Mountains. This river valley sits between three mountain ranges – the Sawatch Range, Mosquito Range, and Sangre de Cristo Range.

Local rockhounds often search the riverbanks and gravel beds for various minerals. The best places to look for Peridot are near the hot springs and in the river gravels. These spots have the right mix of minerals and rocks that often contain Peridot.

What makes this place special is its geology. The area has many hot springs and deep faults that helped create mineral deposits over millions of years.

Besides Peridot, you can find other gems like fluorite, quartz, garnet, and topaz here. Brown’s Canyon and Hecla Junction are popular spots among local gem hunters.

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.