Today I’m sharing close up photos of marvelous malachite. According to geology.com, malachite is a “green copper carbonate hydroxide mineral.” The site also refers to its striking green color and that’s why I collect it.
This first piece has a rough texture and interesting shape. For scale, it measures 1.5 x 1.0 inches.
The second piece is opposite of the first – rounded shapes and smooth textures. It measures 3.75 x 1.5 inches.
The third piece is a cube that’s got interesting lines viewed from different angles. It measures 1.3 x 1.3 x 1.3 inches.
The last piece is an antique watch with a malachite face and band. Malachite has low hardness so it’s relatively easy to work with in making jewelry, carvings, etc. The watch face measures 1.0 x 0.75 inches.
Can you understand why I collect pieces of marvelous malachite? I love its green color and variety of textures.
The following images of igneous rocks up close were taken in my yard near Bend, Oregon.
What’s an igneous rock? Geology.com describes them as being “formed from the solidification of molten rock material.” For example, granite, gabbro, basalt, scoria, and obsidian are all types of igneous rock.
You probably notice some of these rocks have round bubble-like holes in them. These “vesicles” form when gas is trapped within the melted rock at the time it cools and turns solid.
As you can see, there is a lot of variety in texture and color in the igneous rocks in my yard. The rocks pictured are small enough to fit in the palm of my hand – the perfect size for collecting. 😉
On May 18, 1980, a trip to help band golden eagles at the Yakima Canyon in eastern Washington turned into an unexpected Mount St. Helens adventure.
The adventure begins
I was part of the Young Adult Conservation Corps, working for the Washington Department of Game in Olympia, Washington. We spent most of our time in the office, but we took occasional field trips. One of the wildlife biologists invited four of us to help him band eagles and we were excited to get out in the field.
We piled into John’s Volkswagen van and took off for eastern Washington. John suggested stopping at Crab Creek Habitat Management Area, 20 minutes south of Royal City, to do a little birdwatching before driving south to meet the biologist. We stopped and saw yellow-headed blackbirds, cinnamon teal and other kinds of ducks, a short-eared owl, and two Virginia rails with a newly hatched chick.
We drove along the road bordering Crab Creek. There was talk of taking our raft down the creek. Nobody could decide what to do so we pulled off the main road onto a minor side road a half a mile from Smyrna. We had no idea how long we would end up staying on that side road.
We got out of the van to check out the creek and noticed what looked like a storm brewing in the west. John, who was familiar with the area, said that if we rafted the creek, we would see more than we could by car. The rest of us were hesitant about rafting if there was any possibility of rain. As we stood there trying to decide what to do, a “storm” drifted into the valley. John kept saying it wouldn’t matter if we got a little wet and kept insisting we should raft the creek. We still couldn’t decide what to do.
At around 8:30 a.m., we heard what sounded like two sonic booms. We figured the sound came from the nearby Yakima Firing Range, where the United States Army did training exercises. A little while after that, we heard thunder and Dave and I thought we smelled rain. This was Sally’s first time in eastern Washington. She had recently moved from Pennsylvania, and we were busy explaining to her that sometimes big thunderstorms move through eastern Washington. By this time you couldn’t see the far end of the valley and lightning crackled across the sky. John mentioned that he’d gone to college in Ellensburg, an hour west of us, and thunderstorms were common. The rest of us believed him at that point, but we had concerns about the storm.
Uh… that’s not a thunderstorm
The clouds kept moving in until they covered half the sky. Electrical wires overhead buzzed from the electricity in the air. The buzz would get louder until a flash of lightning and a peal of thunder would rock the valley and then the buzz would start again. Meanwhile, the clouds overhead looked like someone had spilled an enormous bowl of gray-colored popcorn and it had spread across the sky. We started talking about how we had never seen clouds like that. Dave, who was from Alabama, said it looked like a tornado sky.
As we talked, the clouds changed again. Now they looked like gigantic fists pounding down on us. By this time, John had given up on rafting the creek and he ran to the van to get his camera. I asked him to grab mine, and we both took pictures of the amazing clouds as they formed overhead. If you followed one it would move downward, exploding into a black haze.
The immense dark clouds now covered about three quarters of the sky. It was dark overhead, and the only light left was in the east. The effect was that of an eerie sunset, but it was 11:00 in the morning. The darkness continued to move across the sky until only a sliver of light remained on the horizon.
At about this time, Sally said she felt something falling on her face. She asked us if we felt it and we said “no” but one by one we felt something falling on us too. John turned on the radio in the van. It said, “In case you haven’t heard, Mount St. Helens has blown.” We looked at each other in disbelief and John let out a hoot and said the mountain “had finally done it.” Several weeks before, we had taken a quick trip to the west side of the mountain for a planned Mount St. Helens adventure. On that trip, we took pictures of the mountain venting steam.
We were excited and didn’t know what to do next. Everyone decided we better get into the van when the ash fall got heavy. It was also getting dark out. The ash was coming down so heavy it was impossible to go out without something covering your mouth. We were 120 miles northeast of Mount St. Helens, directly in the ash’s path. Lightning still flashed every once in a while, spreading in a horizontal direction, like fingers reaching across the sky. The flashes were the only outside light we would glimpse for many hours.
The long dark day
It was so dark you couldn’t see your hand in front of your face. The time was around 11:30 a.m. We didn’t know how long we would be there so we only turned on the radio every once in a while. The disc jockeys were excited about the eruption and played songs like “Volcano” by Jimmy Buffet and “Dust in the Wind” by Kansas. I remember part of Jimmy Buffet’s lyrics in particular: “I don’t know where I’m going to go when the volcano blows.” We had one beer in the van and shared it in a toast to the volcano. We got out a flashlight and spread a map outside to collect ash.
I lit a candle lantern but a little while later we dug out John’s Coleman lantern. We only kept the light on for brief periods of time because it would get too hot in the van. Whenever we opened the window, ash and mosquitoes would pour into the van. We wondered how long we would be in there and what we would do to pass the time.
We talked about what we were experiencing for a while. If we hadn’t been near a radio, we could have thought this was a nuclear explosion and that stuff falling from the sky was radioactive fallout. With the sky being so dark and everything so quiet, it would have been easy to think it was the end of the world. We should have been in a panic, but we were calm about the whole situation. The darkness surrounding us had a kind of presence, but it wasn’t a frightening one.
Okay, now what?
As it became more and more clear that we might be stuck where we were for a while, we started trying to think of things to do. We were lucky we had plenty of food because our plan was to meet four other people and we had enough for everyone for four days. We couldn’t cook anything, but we had plenty of vegetables to snack on and peanut butter and jelly to make sandwiches. Peanut butter and jelly sandwiches were the easiest things to make. Dave, who once worked as a camp counselor, sang us a camp song about the sandwiches in his soft southern drawl.
“First you take the peanuts and you crunch ’em, you crunch ‘em… For your peanut, peanut butter and jelly. Peanut, peanut butter and jelly.”
He cracked us up because of the funny way he sang and danced to the song. Dave pretended to pick grapes, crush peanuts, and spread peanut butter and jelly onto bread. Every time he said the word “jelly” he raised his voice for emphasis. It was easy to imagine how his rendition would entertain young campers.
After that, we started telling dumb jokes and singing camp songs. When we started running out of those, John said he thought he had a deck of cards in the van. He found them, and we played cards for a long time.
We would shut off the light every once in a while because of the heat and to check if it was still dark. It was early afternoon, and the sky was pitch black. When we opened the van door and turned the light on, the mosquitoes and moths would come inside again. We spent a long time trying to get rid of the mosquitoes. They were big ones! As it got later in the day, we thought about sleeping arrangements. We rearranged our gear, including the rubber raft, cooler, and bags of food, to find a place to sleep semi-comfortably.
Meeting some local wildlife
Around this time, we heard a big thud against the side of the van. We looked at each other and when we realized none of us had made the noise, we rushed to lock the doors. I don’t know why, but everyone had the same thought at the same time. We wondered if something had run into the van. John turned on his headlights and we saw a duck lying on the ground. It must have flown into the van because it couldn’t navigate in the darkness. The duck was flapping around like the collision injured it, so I jumped out to check if it was okay. The bird flew off after a couple unsuccessful attempts so it must not have been hurt too badly.
A little while later, when we had the light on, a swallow flew around the windows like it was trying to get into the van. The swallow perched on the windshield wipers for a while and then it would flutter around again. The animals were feeling the effects of the heavy ash fall. John and I thought about the Virginia rail chick we had seen that morning. It was so young it wasn’t yet able to stand. It was likely covered by ash now. We would see more effects on the local wildlife when we woke up the next morning.
By evening we were getting restless and eager for some sign that we would see the light of day again. At around 8:30 p.m., we got a brief glimpse of the landscape. It was light enough to make out the hills surrounding us, but not enough to see very far down the valley. The quick glimpse showed us the ash covering everything, and it was still falling. Dave and John set out a tarp to collect more ash. The map we had laid out earlier had about ¾ of an inch of ash on it. Darkness came again as night fell. The night was quiet and starless.
A new day
We woke the next morning to an unfamiliar world. It was like a layer of gray snow had covered the land. Before, the plants had been green and growing and now they were a pale gray color and bent over from the weight of the ash. The ash covering the ground was nearly two inches deep. The consistency was like baby powder. If you picked up a handful and threw it in the air, it would stay suspended for a while. If you stepped onto it, it was like moon dust. It would whoosh around the sides of your shoe and when you moved your foot away, a deep and perfect print would remain.
As we looked around, there were signs that animals had been very active during the night. Everywhere you looked, you saw tracks. It’s too bad we didn’t have a field guide to animal tracks with us because this would have been the perfect opportunity to use it. Rabbit, mouse, and bird tracks ran in neat lines across the ash. Several tracks formed intricate designs like those of the beetle we observed trudging across this new ash-covered world. It would do loops, turns, stop, and then do it again. Ants tunneled their way out of the thick ash, already adapting to the unfamiliar landscape. An occasional duck would fly by, and a few floated in the nearby creek. The animals were trying to adapt to this altered world, but they didn’t all survive the extended gloomy night.
Making our way towards civilization
We decided we had better try to get out of there and back to civilization. John and Dave picked up the tarp and guessed it held ten pounds of ash. We collected ash in containers and ended up collecting a lot on our shoes and clothing. The ash was still thick in the air and we wore bandanas to help keep it out of our noses and mouths. We took pictures of everyone looking like a bunch of bank robbers.
A couple cars drove by in the distance so everyone decided we should try to get going too. We got in the van to drive to Odessa, an hour and a half to the northeast. The route went up a hill and after we had driven a few miles, the van conked out. It had overheated. This VW van was air cooled, taking air in through collectors on the sides and circulating the air around the engine. The hot, ash-filled air wasn’t cooling the engine down enough. John got mad and took a walk. When he came back, he told us there was an intersection not too far up the hill. Luckily the van started, and we took off towards “civilization.”
Every time a car drove on the roads, it would kick up huge dust clouds that were almost impossible to see through. The main east-west highway in Washington State, Interstate 90, was closed because of the heavy accumulation of ash.
An enormous amount of ash fell at Mount St. Helens, but as it drifted east, accumulations were heavier in certain parts of eastern Washington. We later learned that prior to the eruption, the mountain measured 9,677 feet at the summit. After the eruption, it measured 8,363 feet. A lot of that material had shot up into the atmosphere.
After stopping at a corner store and attempting to call Olympia, we headed for Royal City. The people at the store told us the church there was taking in travelers. The population of Royal City in 1980 was 676 people. We drove to the nearby church and the van almost died again. The van made it to the church and we ended up staying there with about 75 other people for four days.
We donated most of our food to the church so they could share it with the other stranded travelers. The majority of the food served was from the community and there was plenty for everyone. We ate a lot of delicious home-canned vegetables and fruit.
The pastor, his wife, and the sheriff showed great patience in a tough situation. During the last two days of our stay, people were getting antsy to get out of there and they were getting on each other’s nerves. Sally, Dave, John, and I were getting along fine and passed time by telling more dumb jokes.
“Why did the cowboy want a dachshund? So he could get a long little doggie.”
We went to the high school to take showers and once to play basketball and volleyball. As soon as you walked outside, you felt dirty because of the intense heat and the ash floating through the air. Back at the church, the pastor got everyone singing after dinnertime every day to get their minds off the situation. One night they sang “Go Tell It on the Mountain” and then a song about the walls of Jericho tumbling down. I don’t think most people even realized how the songs applied to our predicament.
With the help of the townspeople, we made it through our time in Royal City. They made plans for a convoy with patrol cars, graders, and firetrucks with hoses to help us get back home. Water from the hoses helped to keep the ash down briefly. The convoy would leave the next morning.
The journey home
When we woke up the next morning, the parking lot was almost empty because everyone drove by themselves. We took off with a couple from Seattle following us. It’s good they did because after the van broke down twice in 15 miles, we abandoned it. We left the van at a farm and gave them our food that would have spoiled. The six of us squeezed into the Seattle couple’s compact car and drove to Bellevue, where John’s parents lived. This ride normally took two-and-a-half hours, but it took way longer that day.
John and Dave drove back to get the van the next day. They towed it to John’s parent’s house and worked on it. The ash had been very cruel to the van and unfortunately it would never run again. The van delivered us from our secluded ash-covered camp and worked a couple more times, but it just couldn’t make it the entire way.
When we finally returned to our offices in Olympia, it was like the four of us were joined at the hip. We moved in a herd from room to room. Because of our shared experiences, we couldn’t bear to be apart for a while.
We will always remember this once in a lifetime Mount St. Helens adventure.
Written in May 1980 and edited for clarity.Some names and identifying details have been changed to protect the privacy of individuals.
About the pictures
Today’s Fandango’s One Word Challenge (FOWC) word is “photograph.” I was lucky because I had before, during, and after photographs for this story. I took a lot of pictures when the eruption was happening but I had a little problem. Ash got into my camera and destroyed it. The handful of pictures I was able to save were overexposed. If only I would have had a smartphone!
Sometimes you want to cut a road out of the picture so you can focus on the scenery. I loved the layered land forms at this park.
Other times there’s a sign you overlooked. How did I not see that?
But there are other times when you want to emphasize a sign.
I was interested in that sign because a thunderstorm was about to break. Needless to say, we did not drive down the narrow canyon.
Note: I also used a perspective correction tool in my photo editing program to straighten the sign.
Sometimes a place deserves a more panoramic view so you give it a little trim. You have to decide where the best place is when you’re making the cut. Hope I didn’t cut it too short.
And then there are times when you add a little hidden Easter egg and wonder if anyone will notice it when you share the final cropped photo.
Do you see the tiny tan smudge in the lower left corner on one of the flat rocks? That’s a white-tailed antelope squirrel traveling at Rocky J. Squirrel speed. Not a great picture of it, but good enough that I could identify it later. 😀
When I saw that the Lens-Artists Photo Challenge this week was A River Runs Through It, I immediately thought of the Grand Canyon of the Yellowstone River.
This river meanders its way through colorful rock formations
And pounds down in the Upper Falls
Past pine forests
And into the Lower Falls in the Grand Canyon of the Yellowstone
Artist Thomas Moran captured the river’s spirit in this painting, Grand Canyon of the Yellowstone. He and others on the Hayden Expedition of 1871 traveled to the greater Yellowstone area and documented what they encountered. They were instrumental in the establishment of Yellowstone National Park in March of 1872.
Thomas Moran used his artistic skills to capture outstanding features in vibrant paintings of the landscape. He was an influencer in his time. See more of his work at Painter of Yellowstone.
It’s time once again for fun with photos. Welcome to Photo Bloopers 4! This is what I do with pictures that don’t quite fit in or turned out weird looking. They needed a few words to make them more interesting. Hope they entertain you!
Do you want to see more of my Photo Bloopers? See:
I enjoy visiting Glass Buttes in Central Oregon to collect obsidian. Did you know there are over 24 kinds found there? Here are photos of obsidian up close. The stones are beautiful in color, but also in form.
The Lens-Artists Photo Challenge this week is the five elements of metal, wood, water, fire, and earth. Here are pictures that feature several of the elements that I took at Yellowstone National Park.
The five pictures above of Yellowstone elements each include wood, water, fire, and earth. In this case, the fire is below the surface. This area sits inside a giant caldera and geysers and hot springs are common in the park. Steam rises over these thermal features.
You may be wondering where the element of “metal” is in these photos. In the photo below, I was using our metal car as a blind to take pictures of the bison and accidentally took a picture of myself holding my metal camera. 😀
Hope you enjoy my interpretation of this challenge!
The water in some of the springs presents to the eye the colors of all the precious gems known to commerce. In one spring the hue is like that of an emerald, in another like that of the turquoise, another has the ultra-marine hue of the sapphire, another has the color of topaz; and the suggestions has been made that the names of these jewels may very properly be given to many of these springs.
Nathaniel Pitt Langford in Diary of the Washburn Expedition to the Yellowstone and Firehole Rivers in the Year 1870.
Grand Prismatic Spring is the crown jewel of hot springs at Yellowstone National Park. The landscape of Grand Prismatic has all the colors of the rainbow. The cracks and tracks add some interesting texture as well. This 370-foot wide spring is the largest in the United States and third largest in the world.
The trailhead is 14 miles northwest of Dayville, Oregon. This trail is in the Sheep Rock Unit of the monument. The Island in Time trail is a 1.3 mile long out and back trail with an elevation gain of 200 feet. The Blue Basin Overlook trail also starts here. It’s a 3.25 mile trail with a 760 foot elevation gain. There are several other trails nearby.
The geologic history
The unique blue-green colors of the rock formations in Blue
Basin are stunning. They range from
a pale dinner mint green to a darker, bluer green. The blue-green and tan
claystones and siltstones are part of the John Day formation. There were multiple eruptions of Cascade
Mountain volcanoes 29 million years ago. The ashfall formed the blue-green
layers of this basin. Celandonite and clinoptilolite give these formations
their green color.
You’ll see impressive tiered layers of rock bordering the trail. At the end of the trail, an amphitheater of colorful stone will surround you. I had the place all to myself on my hike. Rotate your way around this photo sphere to see what I saw.
I also noticed the smaller landscapes on this trail. Here are a few of those scenes.
Fossil and facts on Blue Basin trail
You will see several fossil replicas covered with protective plastic bubbles along the trail. They removed the actual fossils to protect them from the elements. Over 2,000 species of plant and animal fossils have been identified in the vicinity.
Map and a word about dogs
Here’s a map of the Blue Basin. Please note the warnings associated with this trail. In the warmer months of the year, you may see rattlesnakes. In October, I saw none. Blue Basin experiences high temperatures in the summer months so be prepared.
There are 13 metal grate bridges on this trail. The sign says dogs may refuse to cross and you may have to carry them. My dog would not cross the first bridge. Sorry, but I couldn’t imagine carrying a 60+ pound dog over 13 bridges. She waited patiently in the car on that cool day.
Amazing paleontology center
Don’t miss the amazing Thomas Condon Paleontology Center while you’re here. The displays impress me and I’m always excited to see paleontologists hard at work in the viewing area. I often wonder what new treasures they will uncover in their daily work.
There are three short hikes near the covered picnic area. The Geologic Time Trail winds along ¼ mile to connect you to the other two trails. Interpretive signs note the changes of the last 50 million years. The colorful small signs explaining the geologic history looked brand new. The Trail of Fossils takes you up a ¼ mile loop trail on the hillside and shows you fossils that left their imprints in large boulders.
An almost-tropical forest covered this region 44 million years ago. 120 inches of rainfall per year, compared to about 9 inches today. Bananas used to grow here! Bear-like predators, four-toed primitive horses, and other creatures once roamed this land. The Clarno Arch Trail takes you up ¼ mile trail (yup, another ¼ mile one!) to the base of a cliff with a natural arch cut into the stone. This trail has a 200 foot elevation gain. If you hike all the trails out and back, it adds up to 1.25 miles.
Spring shrubs and flowers
When I was there in mid-May, wildflowers were in full bloom. The rose bush featured in one of my earlier posts—Wild Rose: Friday Flowers—was near where we parked. The “trunk” of that shrub looked like a formidable weapon! We saw orange globemallow blooming along the trail. Large netleaf hackberry shrubs grew on the slopes near the cliffs.
Birds of the cliffs
There were a handful of birds out that day. Canyon wrens serenaded us with their descending song. A prairie falcon, American kestrel, and golden eagle flew near the cliffs protecting their nest sites. A California quail called Chi-ca-go in the background. Swallows flitted overhead.
Fossilized logs forming a “T” on the cliff face
Logs and lichens
We spotted several fossilized leaves and branches along the Trail of Fossils. When we went up the Clarno Arch Trail, we saw large fossilized logs sticking out of the cliff face. The colorful lichens covering the rocks attracted my attention as usual.
Colorful lichens on the rocks
Stairway to the arch
The columns of the Palisades were formed by volcanic lahars 54-40 millions years ago. They are stately and beautiful but the stair step-like structure beneath the arch really got my attention. Water must have pooled up in each “step” before falling.
Steps beneath the arch
When we were there with Bend Parks and Recreation, it was a cool day. I imagine it gets hot in the summer here so plan your visit with that in mind.
I went on a field trip recently to one of my favorite places–Glass Buttes. Obsidian is everywhere you look! It’s like being a kid in a candy store. In fact in one of my previous posts, Glass Butte Dragonglass, I show a picture of some obsidian I have collected displayed in a candy bowl.
Glass Buttes – Rockhounding and habitat
Located about halfway between the towns of Bend and Burns in eastern Oregon, this site is a rockhounder’s paradise. You can dig and crack open obsidian with a rock hammer, but you really don’t need to because it’s all over the surface. The Bureau of Land Management oversees most of this site. Individuals may collect up to 250 pounds of obsidian per year.
Glass Butte, elevation 6,388 ft., and Little Glass Butte, elevation 6,155 ft., tower over the surrounding hills. Sagebrush, rabbitbrush, and bunchgrass cover the landscape. Western juniper and mountain mahogany are interspersed over the land. Sagebrush-dependent species such as Brewer’s sparrows, sagebrush sparrows, and sage thrashers were seen and heard the day we were there. A pair of mountain bluebirds was seen perching high in the juniper trees. We caught glimpses of ferruginous hawks.
Geological history of Glass Buttes
Glass Buttes formed during the Miocene and Pliocene periods, 5-5.8 million years ago. Three layers of lava flows from volcanic domes and vents formed the buttes. The first flow was basalt, the second rhyolitic lava, and the third another layer of basalt. Rhyolite contains a high percentage of silica and it forms much of the substrate. Due to a rapid rate of cooling of magma at Glass Buttes, larger mineral crystals didn’t have time to form. The silica-rich “glass” of obsidian formed as a result of this process.
Here’s an interesting article with more details about the obsidian at Glass Buttes for you geology geeks. Obsidian is Hot Stuff.
This area is in the Brothers Fault Zone of the High Lava Plains physiographic province. The many faults are easily observed in aerial photos and through the use of Light Detection and Ranging (LiDAR) data. A 2011 map of Glass Buttes based on LiDAR can be seen here.
Flint knappers then and now
Obsidian from Glass Buttes has been used in making tools for thousands of years. Native Americans made arrowheads, spear points, and other cutting tools with the glass-like stone. Obsidian from this site has been found throughout western North America.
Modern day flint knappers take advantage of the abundance of obsidian at this site. Some groups meet annually at events such as the Glass Buttes Knap-in to work on their craft. My first photo on this post shows what flint knappers left behind at one of their campsites.
Obsidian from Glass Buttes, Oregon
Types of obsidian at Glass Buttes
There are MANY types of obsidian at Glass Buttes. I will quote Tim Fisher who runs the Oregon Rockhounds Online website. “Need a list of what’s here? OK, here goes: black/mahogany, leopardskin, mahogany, Midnite lace, triple flow, double flow, pumpkin, purple and silver sheen, gold sheen, silver sheen, rainbow, peacock, purple sheen, fire, green, Aurora Borealis rainbow, black, opaque black, opaque banded, gunmetal, and probably many more!” If you want detailed information on where to find the different types, please purchase the Ore Rock On guide from his website. We own it and it contains invaluable info for sites in Oregon, Washington, Idaho and western Montana.
Some rockhounds search for specific types, such as rainbow and fire obsidian, and they can be the most difficult to find.
Exploratory geothermal site
Other land use
We made a couple additional short stops on the field trip. We stopped at an abandoned mercury-bearing cinnabar mine. The site was discovered in 1933 and mined until 1957. Another stop was made at an exploratory geothermal well site. No development is currently taking place but it may happen in the future. Greater sage-grouse live and breed here and that may limit development.
This is a great area to visit but I should remind you of a couple things. Obsidian is SHARP so make sure you have good tires and a spare tire. Four-wheel drive vehicles are recommended for certain areas. There is no water or facilities here. If you visit, be prepared. Access to this site is on an unmarked road near mile marker 77 on Highway 20. Drive south a couple miles to find obsidian. Additional information is available from the organizations listed here.
I have been to this site several times. My recent trip was with Bend Parks and Recreation. I always wish I could stay at Glass Buttes just a little bit longer. It’s a hard place to leave if you love rocks!
To see some of the obsidian I have collected at Glass Buttes over the years, see:
Today I took a hike up Gray Butte, northeast of Terrebonne, Oregon. It was a nice hike with lots of wildflowers and spectacular views. This view is from the edge of the Crooked River Caldera looking west to Mount Jefferson, on the right, and Black Butte, on the left. The rocks in the foreground are splattered with messages left by lichens.
My place in the world is out in the wild places of central Oregon. From dry sagebrush steppe in a caldera to lush meadows bordered by pine forests. There are so many special places to explore…