πͺ¨ FREE ROCKHOUNDING GUIDE #2
Clear Lake Obsidian Country
Lake County, California
Guide type: Geology, identification, ethical scouting, and legal collecting
Best for: Obsidian enthusiasts, volcanic-rock collectors, families, and geology-curious adventurers
Important: Clear Lake has exceptional obsidian, but it does not currently have a clearly designated public obsidian-collecting site comparable to an established rockhound area.
β οΈ Important Location Update
Clear Lakeβs best-known obsidian sources are associated with Borax Lake and Mount Konocti. These areas overlap private property, culturally significant Indigenous landscapes, and archaeological sites containing thousands of years of human history.
This guide intentionally does not publish quarry coordinates or direct visitors onto Borax Lake archaeological ground. Ancient flakes, cores, projectile points, and worked obsidian are artifacts, not rockhounding souvenirs. Archaeological material found on federal land must be left exactly where it lies.
The goal is to understand Clear Lake obsidian, recognize naturally transported pieces, and collect only where land ownership and regulations clearly permit it.
π Where Is It?
Clear Lake lies in Lake County within the Clear Lake Volcanic Field, approximately 90 miles north of San Francisco. The volcanic field includes Clearlake, Lower Lake, Kelseyville, Lakeport, Lucerne, Mount Konocti, Borax Lake, and portions of the surrounding hills.
Use Lower Lake, California as the practical navigation hub for the southeastern side of the lake.
Geology and history stop
Anderson Marsh State Historic Park
Located along Highway 53 between Lower Lake and Clearlake.
This is an excellent place to understand the lake basin, marsh environment, and Indigenous history, but it is a look-and-learn stop, not a collecting stop. The park protects archaeological sites and a cultural landscape connected to the Koi people. California State Park regulations generally prohibit disturbing or removing rocks, minerals, gravel, or archaeological material unless a unit is specifically designated for rockhounding.
As of July 2026:
- Open sunrise to sunset
- Vehicle day-use fee listed as $4
- Dogs are not permitted
- Temporary fire restrictions may be active
Potential legal scouting area
Knoxville Management Area
This large BLM-managed area lies southeast of Clear Lake and can be approached using Morgan Valley Road. The BLM map shows public parcels intermingled with non-BLM property, so an offline land-ownership map and active GPS are essential. The area contains rugged roads, former mining country, volcanic-related geology, and substantial private-property boundaries.
Obsidian is not guaranteed at Knoxville. Treat it as a public-land volcanic-rock scouting area rather than a proven obsidian bed.
Before collecting, contact the BLM Ukiah Field Office at 707-468-4000 and ask:
βIs casual collection of naturally occurring obsidian currently permitted on BLM parcels in the Knoxville Management Area, and are there any closed areas, active claims, cultural-resource restrictions, or fire restrictions I should know about?β
That phone call is the difference between rockhounding and accidentally starring in CSI: Volcanic Glass Unit.
π« Places That Are Not Collecting Locations
Do not collect from:
- Borax Lake archaeological property
- Anderson Marsh State Historic Park
- Mount Konocti preserves, parks, or private parcels without written permission
- Vineyards, ranches, orchards, or vacant-looking private land
- Active mining claims
- Developed recreation sites
- Mine dumps, tailings, tunnels, adits, or remediation areas
- Locations containing worked flakes, projectile points, cores, grinding features, or concentrations of obsidian debris
A fence is not required for land to be private, and a missing sign is not permission.
π The Geology
Clear Lake is not merely sitting near an old volcano. It occupies the middle of a broad, geologically active volcanic system.
The Clear Lake Volcanics range from approximately 2.1 million years old to about 8,500 years old. Their compositions range from basalt to rhyolite, although rhyodacite is the fieldβs most voluminous rock type. Volcanism has become increasingly concentrated south and east of the lake during the past million years.
Mount Konocti is a predominantly dacitic volcanic complex approximately 300,000 years old. The youngest known eruptions around Clear Lake occurred roughly 8,500 to 13,500 years ago, producing maar craters, ash, volcanic bombs, and other explosive deposits around the southeastern lake basin.
How the obsidian formed
Obsidian forms when silica-rich lava cools without allowing enough time for an orderly crystal structure to develop. Instead of becoming visibly crystalline rhyolite, part of the lava freezes into volcanic glass.
Clear Lake contains two especially important geochemical obsidian sources:
Borax Lake obsidian
Associated with a rhyolitic flow approximately 90,000 years old. It is commonly dark gray to black and may have a gray, frothy appearance caused by small gas voids.
Mount Konocti obsidian
Associated with volcanic units south of Mount Konocti. Documented colors include gray, black, brown-black, and brick-reddish brown.
Erosion can move pieces away from their original flows and place obsidian pebbles in younger gravel, alluvium, creek deposits, and old lake sediments. That transported material is called float. Finding legal, naturally transported float is the safest goal for a recreational collector.
π What Natural Obsidian Looks Like
Look for these characteristics together rather than relying on color alone.
Glassy luster
A fresh surface reflects light like dark glass. Weathered surfaces can become dull, cloudy, gray, brown, or lightly crusted.
Conchoidal fracture
Obsidian breaks in smooth, curved surfaces resembling overlapping shells. Ripple marks may radiate away from the impact point.
Razor-sharp edges
Fresh fractures can be considerably sharper than ordinary stone. Never sweep loose fragments with your bare hand.
Translucent thin edges
Hold a thin edge in front of a flashlight or bright sky. Black obsidian may glow smoky gray, brown, amber, or reddish along its thinnest edge.
Natural cortex
A naturally weathered piece may have a dull, pitted, brown, gray, or chalky outer rind covering a glassy interior.
Flow texture
Some pieces display faint bands, streaks, folded lines, tiny bubbles, or changes in translucency created while the lava was moving.
π§΄ Obsidian or Bottle Glass?
Clear Lake recreation areas contain modern glass too, and yesterdayβs soda bottle is rarely a Pleistocene eruption.
Obsidian is more likely when:
- It occurs with other volcanic rocks
- Several surfaces have a weathered natural rind
- The fractures are irregular and multidirectional
- Flow bands or natural inclusions are visible
- The piece appears embedded in undisturbed gravel or volcanic soil
Manufactured glass is more likely when:
- It is bright green, cobalt blue, or perfectly clear
- It has uniform thickness
- One face is perfectly flat or curved like a bottle
- Lettering, mold seams, bubbles, or machine-made ridges are present
- It occurs with cans, ceramics, or modern trash
Color by itself is not a reliable test.
β Rare or Unusual Finds
These are possible regional varieties, not guaranteed finds.
Reddish-brown Konocti-type obsidian
Brick-red, brown-black, or reddish translucent material is less common than ordinary black volcanic glass and can be visually striking. Confirming the source requires geochemical testing rather than appearance alone.
Frothy gray Borax Lake-type obsidian
Some Borax Lake material contains small gas voids that give it a gray, bubbly, or slightly foamy appearance.
Flow-banded volcanic glass
Alternating glossy and cloudy layers may preserve movement within the cooling lava.
Obsidian breccia
Angular glass fragments can become enclosed within volcanic material during repeated breaking, movement, and cooling. The Clear Lake sources include massive flows, domes, and brecciated volcanic units.
Volcanic companions
The wider field can also contain:
- Rhyolite and rhyodacite
- Dacite
- Basalt and basaltic andesite
- Scoria and vesicular lava
- Pumiceous or ash-rich material
- Hydrothermally altered volcanic rock
These are part of the same volcanic orchestra, even when obsidian gets the guitar solo.
π§ Where to Examine the Ground
Only use these methods after verifying that you are on land where collecting is permitted.
1. Naturally eroded gravel
Examine loose gravel that has already weathered from slopes. Dark glassy pieces often stand out after rain has washed away dust.
2. Dry drainage margins
Search loose material along the upper edges of washes rather than disturbing banks or digging into sediment.
3. Erosion below volcanic slopes
Obsidian is more likely to survive as angular float close to its source. Farther downslope, pieces become smaller, rounder, and more weathered.
4. Old alluvial gravel
Naturally transported obsidian may occur as rounded or subangular pebbles mixed with basalt, rhyolite, chert, sandstone, and other regional rock.
5. Previously disturbed legal surfaces
On confirmed BLM land, examine loose material beside existing routes or previously disturbed ground without widening roads, cutting vegetation, or entering closed areas.
Do not hammer cliffs, roadcuts, archaeological deposits, or bedrock exposures beside public highways.
πͺΆ The Artifact Rule
Clear Lake obsidian was used by Indigenous communities for thousands of years. Natural obsidian and worked obsidian can occur in the same general landscape.
Stop immediately when you see:
- Repeated flake scars
- A deliberately shaped edge
- A symmetrical point or blade
- A rounded striking platform
- Numerous flakes concentrated together
- Grinding stones, shell, bone, charcoal, or pottery
- Obsidian positioned beside other cultural material
Do not pick it up to βcheck whether it is real.β Photograph it where it lies, preserve the location, and report it to the relevant land manager. Moving an artifact even a few feet destroys archaeological context.
π Suggested Gear
- Leather gloves resistant to sharp edges
- Safety glasses
- Sturdy boots
- Long pants
- Ten-power hand lens
- Small flashlight for testing translucency
- White index card for viewing edge color
- Hard plastic specimen container
- Newspaper or individual sample bags
- Permanent marker and locality labels
- First-aid kit with gauze and wound dressings
- Official BLM map plus offline GPS
- Plenty of water
- Fire extinguisher during dry season
Leave the rock hammer packed away until collection rights are completely confirmed. Loose float is enough for a productive scouting trip.
β οΈ Collection Rules
On ordinary BLM-managed California land, casual collection may be permitted when specimens are for personal, noncommercial use and the area is not closed, claimed, developed, privately owned, or otherwise restricted.
California BLMβs general limit is:
- Up to 25 pounds per day, plus one additional piece
- No more than 250 pounds per person per year
- Hand collection only
- No commercial collecting or bartering
- No unnecessary damage to the land
- No collecting from archaeological sites or active mining claims
Important for The Hidden Gem
Material collected under BLM casual-use rules is personal-use material. It should not be placed into shop inventory, sold, traded for business benefit, or incorporated into products for profit. Commercial sourcing requires separate authorization or material acquired from a lawful private source.
β οΈ Mercury and Mine Safety
The Clear Lake region has a long history of mercury mining. Sulphur Bank Mine on the eastern shore is a federal Superfund site, and mercury contamination remains an environmental concern around the Oaks Arm of Clear Lake.
Avoid:
- Sulphur Bank Mine property
- Mine tailings and calcined ore
- Yellow, orange, or unusually powdery mine waste
- Warm springs and gas vents
- Abandoned structures
- Tunnels and adits
- Water draining from mine workings
- Dusty material around historic mercury sites
Do not cut, grind, tumble, or polish material suspected of coming from a mercury-mine area until its origin and safety are understood.
π₯ Seasonal Safety
As of July 2026, the BLM Ukiah Field Office has an active fire-prevention order due to increased wildfire danger. Conditions and restrictions can change rapidly. Check before every visit, even when you were there recently and everything looked peaceful. Dry California grass can transform from scenery into a fuse with alarming enthusiasm.
Also prepare for:
- High summer temperatures
- Limited cellular reception
- Rattlesnakes and ticks
- Sharp volcanic glass
- Rough, two-way dirt roads
- Hunting activity
- Sudden road closures
- Private-property boundaries
π Why California Is a Rockhound's Paradise
(And Why We Don't Need to Tell You Our Favorite Spot π)
If you asked a geologist to design the perfect place for rockhounding...
They might accidentally invent California.
Seriously.
Few places on Earth pack this much geological variety into one state.
ποΈ Towering mountain ranges.
π Ancient volcanoes.
π Rugged coastlines.
ποΈ Vast deserts.
π² Forests.
βοΈ Historic mining districts.
Millions upon millions of years of Earth's history are written across California's landscape.
Every region tells a different story.
π Fire Built It
Ancient volcanoes poured rivers of lava across parts of California.
As that molten rock cooled, it created incredible volcanic landscapes and the minerals collectors love today.
ποΈ Mountains Lifted It
Gigantic forces deep inside the Earth pushed mountains toward the sky.
Those same forces exposed rocks that had been hidden for millions of years.
Imagine turning the pages of a book that Earth wrote over hundreds of millions of years.
That's what mountain building does.
π Water Shaped It
Rivers carved canyons.
Oceans polished stones.
Winter storms moved boulders.
Glaciers sculpted valleys.
Nature has been the world's greatest lapidary artist for a very long time.
π Treasure Is Everywhere...
California is famous for producing incredible minerals and gemstones, including:
β¨ Quartz
π Agates
π¨ Jasper
π€ Obsidian
π Gold
π Tourmaline
π Jade
π£ Benitoite
...and countless others.
Every trip into the field has the potential to surprise you.
π€« "So... Where Do You Go?"
That's probably the question we hear more than any other.
Here's the truth:
The best rockhounds don't just collect rocks...
They earn their discoveries.
They study maps.
Learn geology.
Explore responsibly.
Respect private property.
Leave places cleaner than they found them.
And sometimes they spend an entire day outdoors without finding anything spectacular...
Only to uncover something unforgettable on the next trip.
That's part of the adventure.
At The Hidden Gem, we'll happily teach you how to become a better rockhound.
But some special locations are protected out of respect for the land, the people who discovered them, and future generations of explorers.
Great rockhounds don't just protect their finds.
They protect the places that made those finds possible.
π§ Hidden Gem Thought
The greatest discovery isn't finding someone else's secret location...
It's finding your own. but our members are def gonna learn our spots :)
That first place you'll always remember.
The one you found through curiosity, patience, and a little dirt under your boots.
Those are the stories worth telling.
π Community Question
What's your favorite thing about rockhounding in California?
ποΈ The mountains?
π The coastline?
ποΈ The desert?
π² The forests?
βοΈ The history?
(No GPS coordinates, please. π Let's keep the magic alive.)
β€οΈ Why Adults Need Hobbies Again
When you were a kid...
A stick became a sword.
A creek became an expedition.
A cool rock became treasure.
Somewhere along the way, life got busy.
Work.
Bills.
Meetings.
Notifications.
Deadlines.
We stopped exploring and started scrolling.
Then something funny happens...
You bend down to pick up one interesting rock.
Suddenly you're asking:
"What mineral is this?"
"How old is it?"
"How did this form?"
Before you know it, you've spent three hours outside without thinking about work once.
That's the magic of rockhounding.
It slows the world down.
There's no race.
No inbox.
No high score.
Just fresh air, curious eyes, and the possibility that your next step could uncover something that has been hidden for millions of years.
πͺ¨ Rockhounding Isn't About Collecting Rocks
It's about collecting moments.
π Watching the sunrise over a mountain.
π₯Ύ Hiking somewhere you've never been.
π Laughing because your backpack somehow weighs twice as much on the way back.
π€ Meeting people who get excited over a shiny rock sticking out of the dirt.
π Learning a little more about our incredible planet every time you head outside.
The rocks are simply the souvenirs.
π Hidden Gem Perspective
The Earth has been creating masterpieces for over 4.5 billion years.
Every expedition is a chance to discover one that nobody else noticed.
Not because it's valuable...
But because you found it.
π¬ A Question Worth Asking
If someone gave you an entire day with:
β No phone calls
β No emails
β No meetings
Where would you go?
ποΈ The mountains?
π The beach?
ποΈ The desert?
ποΈ A quiet creek?
Tell us where your perfect rockhounding day would begin.
Because sometimes the greatest thing you'll find isn't a crystal...
It's a little piece of yourself that got left behind in childhood.
βοΈ Welcome back to exploring.
π Every Rock Has a Birth Story
Meet the Three Families of Rocks
Believe it or not...
Every rock on Earth belongs to one of three families.
That's it.
Once you understand these three, you'll never look at a mountain, river, or beach the same way again.
Let's meet them.
π₯ 1. Igneous Rocks
"Born from Fire"
Igneous rocks begin life as molten rock (magma or lava).
When that molten rock cools...
A brand-new rock is born.
Think of them as Earth's original construction workers.
Examples:
π€ Obsidian
βͺ Granite
π©Ά Basalt
π Pumice
Fun Fact:
The Sierra Nevada Mountains are made mostly of granite that formed deep underground from giant magma chambers millions of years ago.
π 2. Sedimentary Rocks
"Built One Grain at a Time"
Imagine rivers carrying tiny pieces of rock.
Those grains settle.
More pile on top.
Pressure squeezes them together...
And eventually they become solid rock.
Nature's version of making the world's biggest layered cake.
Examples:
π€ Sandstone
βͺ Limestone
π« Shale
Many fossils are found in sedimentary rocks because ancient plants and animals were buried by mud and sand before they could decay.
If rocks kept photo albums...
Sedimentary rocks would have the most pictures.
ποΈ 3. Metamorphic Rocks
"The Ultimate Makeover"
Some rocks don't stay the same.
Deep underground they're exposed to incredible heat and pressure.
They don't melt...
They transform.
Like a caterpillar becoming a butterfly...
Except with significantly fewer wings.
Examples:
β¨ Marble
π Serpentinite
β« Slate
π©Ά Gneiss (pronounced "nice"... because geology enjoys keeping us humble.)
π€― Hidden Gem Mind Bender
A rock doesn't have to stay in one family forever.
Granite can weather into sand.
That sand can become sandstone.
Sandstone can transform into quartzite.
Quartzite can melt and become magma...
Which cools into a brand-new igneous rock.
It's called the Rock Cycle, and it's been running for billions of years.
Earth is the ultimate recycler.
πͺ¨ Hidden Gem Challenge
Look at the nearest rock you can find.
Which family do you think it belongs to?
π₯ Igneous
π Sedimentary
ποΈ Metamorphic
Drop your guess below!
You might be surprised how much of a geologist you're already becoming. βοΈπ
π¦ Did Dinosaurs Ever See Your Rock?
It's one of the most common questions we hear at The Hidden Gem.
"Were dinosaurs around when this rock formed?"
The answer?
Sometimes... and sometimes not even close.
Let's play a game.
π Obsidian
Dinosaurs? β Nope.
Obsidian forms when lava cools extremely quickly after a volcanic eruption. Most obsidian you'll find is less than a few million years old, making it far too young for dinosaurs.
Translation:
A T. rex never admired your obsidian arrowhead.
π Amethyst
Dinosaurs? β Usually!
Many amethyst deposits formed 100 to 300+ million years ago, which means plenty of dinosaurs were roaming the Earth while these crystals were quietly growing underground.
Imagine a giant sauropod walking overhead while your crystal slowly formed beneath its feet.
π Agate
Dinosaurs? π€ Maybe!
Agates formed during many different periods in Earth's history.
Some agates are older than dinosaurs.
Some formed while dinosaurs ruled the planet.
Others are much younger.
Every agate has its own story.
π² Petrified Wood
Dinosaurs? π¦ Very possible!
Many pieces of petrified wood came from forests that grew while dinosaurs were alive.
Some dinosaurs may have literally walked through those ancient forests before the trees became stone.
That's about as close to time travel as you can get.
β°οΈ Granite
Dinosaurs? β Not even close.
Much of the granite in places like the Sierra Nevada formed 80 to 120 million years ago, while some granite elsewhere on Earth is over 3 billion years old.
That means some granite was already ancient before the very first dinosaur hatched.
Let that sink in.
π€― Hidden Gem Mind Bender
If Earth's entire history were a 24-hour day...
π¦ Dinosaurs wouldn't appear until around 10:40 PM.
π£ Modern humans wouldn't arrive until the last few seconds before midnight.
We've barely stepped onto the stage.
The rocks have been here almost the entire show.
π Hidden Gem Challenge
Look around your house.
Pick your favorite rock or crystal.
Do you think it's:
π’ Older than dinosaurs?
π‘ From the dinosaur age?
π΅ Younger than dinosaurs?
Take your best guess below, and we'll help you figure it out!
Because every rock has a birthday...
Some are just easier to celebrate than others. πͺ¨π
βοΈ 10 Things I Wish Someone Had Told Me Before I Started Rockhounding
Every experienced rockhound remembers their first trip...
And every experienced rockhound has made at least a few of these mistakes. π
If you're new to the hobby, consider this your shortcut.
1. Every Rock Looks Interesting.
Spoiler alert...
Most of them are.
Curiosity is a superpower in this hobby.
2. Don't Judge a Rock by Its Outside.
Some of the most spectacular agates, thunder eggs, and geodes look like ordinary gray potatoes until they're cut open.
Nature loves surprises.
3. The Best Finds Usually Require Walking.
The parking lot has already been picked over.
If you're willing to hike just a little farther than everyone else, your odds of finding something special go way up.
4. Always Look Down...
But Don't Forget to Look Up.
Amazing rocks are under your feet.
Poison oak, low branches, cliffs, rattlesnakes, and uneven ground are everywhere else.
A great rock isn't worth a trip to the emergency room.
5. Bring More Water Than You Think You'll Need.
The rocks have been waiting millions of years.
You don't have to race them.
Take breaks.
Stay hydrated.
Enjoy the journey.
6. Ask Permission.
Respect private property.
Follow collecting rules.
Leave every place better than you found it.
Being a great rockhound also means being a great steward of the land.
7. Take Pictures Before You Pick It Up.
You'll never regret having a photo showing exactly where and how you found an amazing specimen.
Years later, those pictures become part of the story.
8. You Don't Need to Bring Everything Home.
Take the exceptional specimens.
Leave plenty for someone else to discover.
A good collection is built with quality...
Not quantity.
9. Every Rock Has Something to Teach You.
Even if it's not valuable.
Every specimen helps you recognize textures, minerals, colors, crystal habits, weathering, and geology.
There really are no wasted finds.
10. The Best Part Isn't the Rocks.
It's the adventure.
The sunrise.
The conversations.
The quiet.
The excitement when someone yells,
"I FOUND SOMETHING!"
That's what keeps us coming back.
The rocks are simply the souvenirs.
π Hidden Gem Thought
Rockhounding isn't about finding treasure every trip.
It's about becoming the kind of person who notices the treasure that everyone else walks right past.
π What's one lesson rockhounding has taught YOU?
Share it below and help the next generation of explorers.