If you love gemstones, Missouri is the place to be for finding beautiful peridot. From famous spots like the Ozark Mountains to hidden places like Marble Hill, you can hunt for peridot all across the state.
Searching for peridot is an exciting adventure that lets you enjoy Missouri’s stunning outdoors. Popular places like St. Francis River and secret spots in the St. Francois Mountains are perfect for discovering this gorgeous green gem. Now, let’s check out other popular peridot spots
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
Always Confirm Access and Collection Rules!
Before heading out to any of the locations on our list you need to confirm access requirements and collection rules for both public and private locations directly with the location. We haven’t personally verified every location and the access requirements and collection rules often change without notice.
Many of the locations we mention will not allow collecting but are still great places for those who love to find beautiful rocks and minerals in the wild without keeping them. We also can’t guarantee you will find anything in these locations since they are constantly changing.
Always get updated information directly from the source ahead of time to ensure responsible rockhounding. If you want even more current options it’s always a good idea to contact local rock and mineral clubs and groups
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 Missouri, the peridot stones you can find are bright and colorful, ranging from yellow-green to olive tones. They often look like Arizona peridots, with their beautiful lime-green hues that really shine in the sunlight.
The peridots here are usually smaller than those from other places, but they still have great clarity and sparkle. We’ve talked with miners who discovered many of them in volcanic areas like the St. Francois Mountains, where they’re nestled in basalt rock.
Some Great Places To Start
Here are some of the better places in the state to start looking for peridot:
Always Confirm Access and Collection Rules!
Before heading out to any of the locations on our list you need to confirm access requirements and collection rules for both public and private locations directly with the location. We haven’t personally verified every location and the access requirements and collection rules often change without notice.
Many of the locations we mention will not allow collecting but are still great places for those who love to find beautiful rocks and minerals in the wild without keeping them. We also can’t guarantee you will find anything in these locations since they are constantly changing.
Always get updated information directly from the source ahead of time to ensure responsible rockhounding. If you want even more current options it’s always a good idea to contact local rock and mineral clubs and groups
St. Francois Mountains
The St. Francois Mountains in Madison County are a great place to look for peridot. Focus on the rhyolite and granite rock formations, where peridot often hides in the cracks.
To find the best spots, head to old mining areas and check the weathered rocks for hidden gems. A hammer and chisel can help, and remember to check if rockhounding is allowed in the area.
Iron Mountain
Iron Mountain in southeastern Missouri is a great spot for finding peridot. The area is filled with rhyolite, a volcanic rock where peridot is often found, especially in cracks and weathered spots.
To improve your chances, try searching near old mining sites where erosion has exposed hidden minerals. Always remember to follow local rules and regulations before collecting.
Central Missouri Barite District
The Central Missouri Barite District is a great place for rockhounds looking for peridot. This area is famous for its rich deposits of barite, but it’s also known for its hidden treasures, like peridot. The peridot in this district forms in the cracks and veins of the rocks, often mixed in with other minerals.
One of the best tips for finding peridot in the Central Missouri Barite District is to carefully check out the barite deposits. Peridot often forms alongside other minerals like quartz or pyrite, so it helps to know what to look for.
The district is large, so it’s important to focus on areas that are known for having exposed mineral veins, like along old mining sites or around the edges of hills.
Marble Hill
Marble Hill in Missouri is a fantastic place for rockhounds to hunt for peridot. This area is known for its rich geology, with rocks and soil full of minerals that have formed over millions of years. The cool thing about Marble Hill is that peridot can be found in a variety of sizes, so you never know what you might discover.
What makes Marble Hill even better is how accessible it is for rockhounds of all levels. It’s a perfect place for a fun adventure, and since it’s not super crowded, there’s a good chance of finding some amazing peridot stones to add to your collection.
Monett
Monett, in southwestern Missouri, is a promising spot to search for peridot. The mineral-rich soil and unique geology of the area create opportunities to find small pieces of this rare stone, especially in streams and gravel beds.
Look for peridot in gravel bars and streambeds, particularly after heavy rain, which can uncover new materials. Tools like a sifting screen or sluice box help separate the greenish-yellow peridot from other rocks, but patience is key since the stones are often small and unpolished.
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.
County | Location |
Benton | Cole Camp |
Crawford | Steeleville |
Callaway | Fulton |
Cape Girardeau | Mississippi River |
Franklin | gravel pits and road cuts |
Jefferson | in gravel and volcanic deposits |
Lincoln | Missouri River |
Madison | St. Francis River |
St. Louis | quarries and road cuts |
Wayne | Road cuts and glacial deposits |
Carter | Van Buren |
Douglas | local gravel pits |
Howell | West Plains |
Madison | old mining sites |
Reynolds | Mine La Motte |
Washington | local quarries and road cuts |
Osage | Missouri River |
Ozark | Meramec Highlands |
Laclede | near Lebanon |