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!
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…
Here’s one more entry for the Weekly Photo Challenge of Lines. The many layered castles in Bryce Canyon National Park are an amazing sight. A single hoodoo formation is impressive, but when you see hundreds of them in lines like soldiers standing at attention, they are just plain stunning.
See my previous post Time Lines: Utah Parks for more pictures featuring a small taste of the geology in Utah’s parks.
I have so many Yellowstone favorite places it’s hard to choose. Here’s a collection of photos of things that make the park special. I start this post with a quote from President Theodore Roosevelt who was known as the “conservation president.”
“The only way that the people as a whole can secure to themselves and their children the enjoyment in perpetuity of what the Yellowstone Park has to give is by assuming the ownership in the name of the nation and by jealously safeguarding and preserving the scenery, the forests, and the wild creatures.”
Theodore Roosevelt, April 24, 1903 at the laying of the cornerstone of Gateway to Yellowstone National Park
Yellowstone National Park, with its larger-than-life landscapes, dramatically changing weather conditions, amazing menagerie of wildlife, variety of plant life, and geology in action, is one of my favorite places. It also has a rich history as the world’s first national park.
A park is born
Evidence shows ancient peoples lived in Yellowstone Country 11,000 years ago. European Americans began exploring the lands in the early 1800’s. Teams of explorers brought back tales of wonder of this unique environment. Their work was supported by images created by artists Thomas Moran and Henry W. Elliot and photographer William Henry Jackson. The park was established in 1872 by President Ulysses S. Grant. Additional protections for the park and its wildlife were instituted in 1894 when congress passed the National Park Protection Act – now known as the Lacey Act.
President Theodore Roosevelt had a love of the land and he was instrumental in making sure many natural areas were preserved. His quote above reflects the importance of preserving wild places so that all may enjoy them “in perpetuity.”
Landscapes – large and small
Here are photos of some special landscapes.
Grand Prismatic Spring, Yellowstone National Park
And more of spectacular hot springs and other features.
And don’t forget to notice the tiny landscapes beneath your feet.
And of course the wildlife.
Yellowstone National Park gets visitors from all over the world. 4,116,524 people visited in 2017.
May we all continue to safeguard and preserve its scenery, forests, and wild creatures.
Do you ever drive by a place a million times and think to yourself, “I’ve got to stop there one day.” This rockshop, south of Redmond, Oregon, was one of those places for me. We finally stopped last summer. The shop has hundreds of carefully labeled rocks inside and out.
Canutts Gem and Rockshop display room
There are a wide variety of rocks in Central Oregon and this shop displays some of the beauties collected over the past 42 years by the owner. Owners Mel and Jerry Lindbeck obviously have a love of rocks. Mel shapes some of the rocks into spheres, bookends, and display pieces.
Canutts Gem and Rockshop
Lovely displays of rocks
We have been to plenty of rock shops over the years but this one displays them in lovely ways. The front room has a couple display cabinets, a table with small rocks, and windows lined with slices of semi-transparent agate.
Canutts Gem and Rockshop displays
The back room is filled with neatly arranged specimens. In other rock stores we have visited, dust and dirt seem to be part of the collection. Not here. The polished spheres shine and sparkle, reflecting the light. The many amazing specimens invite you to take a closer look.
Canutts Gem and Rockshop outside displays
This is a good place to see some of the rock native to this area. Inside you can see thundereggs, petrified wood, jasper, agate, obsidian, and less common things such as Hampton green petrified wood. Outside you will see some of these same types of rock in boulder-size specimens. You will also see smaller specimens of some of the rocks in water-filled birdbaths that bring out their color. Rough rock is also on display outside in big piles.
Canutts Gem and Rockshop outside displays
And more rocks…
Canutts Gem and Rockshop outside displays
Though most of the rock is from Central Oregon in this shop, there are specimens from elsewhere as well. Pyrite, malachite (one of my favorites), lapis lazuli, copper, quartz, and fossils are all represented. Click here and scroll to the bottom of the page to see the owner’s sense of humor about a special fossil in their collection.
So if you like rocks, think about stopping at this roadside attraction on Highway 97. To find out more about the shop, go to Canutts Gems and Rockshop.
Canutts Gem and Rockshop roadside sign
Please support our local businesses and buy rocks for yourself, friends, and family. Remember, a rock makes a special gift that lasts forever.
The Weekly Photo Challenge this week is Structure. I immediately thought of our recent trip to the five national parks in Utah. The structure of the rocks and geological features is complimented by the trees in these parks. Whether dead and twisting, or green and contrasting, the trees are a main character in an interesting landscape.
Arches National Park, Utah
The arches are amazing at Arches National Park and standing dead trees add to the scene. You can see Double Arch in the background.
A fence along the trail in Canyonlands National Park, Utah
I loved these fences made from old juniper wood in Canyonlands National Park. They helped keep people on the trail and were nice to look at too.
Capitol Reef National Park, Utah
The rainbow of colors in the cliffs of this canyon in Capitol Reef National Park were complimented by the bright green of the trees. A storm was moving in in this picture.
Bryce Canyon National Park, Utah
A windswept pine tree clings to the edge of a cliff in Bryce Canyon National Park. Puffy white clouds (like in “The Simpsons” cartoons) float gracefully in the background.
Zion National Park
Colorful and tilting structures in the rock, line a tree-filled canyon in Zion National Park. A few wispy clouds hang over the valley.
The national parks in Utah are full of interesting structures both large and small. The geology of the region tells a dramatic story. The trees and other plants living here have adapted to harsh conditions. The wildlife living here takes advantage of the local environment.
Take the time to look up but also to look down when you visit these parks. Each park is a little different from the others and each one has amazing sights worth seeing. The forces of Nature are strong here.
The Otter Bench Trail gives you some breathtaking views of the Crooked River. The trail head is near the town of Crooked River Ranch and the trail goes along the base of the cliffs bordering the river. We walked a couple miles in, stopped for lunch, and then headed back. There is little elevation change on the section we hiked but if you decide to head down to the river, it gets steep.
The trail goes through juniper and sagebrush habitat and along rocky talus slopes. If you go off the trail a little ways, you can walk to the edge of cliffs that enclose the river far below. If you have a fear of heights, don’t get too close to that edge. A turkey vulture flew by at eye height when we were close to the edge. Hope it wasn’t waiting for a meal!
You get a good view of some of the geological forces at work here. The basalt columns in the lower cliffs are part of the Deschutes formation. Above them you can see light tan colored tuff. Far above the tuff area you will see more columnar basalt and it is part of the most recent Newberry formation.
There is a small dam on the river a few miles from the trail head.
There are golden eagles nesting on the cliffs and you can see how easy it was for them to find a nest site here. The Horny Hollow Trail forks off from the main trail but it’s closed seasonally when the birds are nesting. It was closed when we were there but I saw eagles flying above the highest cliffs in the distance.
I heard and saw quite a few songbirds on this hike in April. The list of species seen includes Townsend’s solitaire, black billed magpie, mountain chickadee, Brewer’s sparrow, and western meadowlark. It was nice to hear some of these songsters again.
As temperatures begin to warm up, the high desert starts its wildflower show. We saw big showy arrowhead balsamroot, purple phlox and rock cress, delicate pink prairie stars, yellow fiddleneck, larkspur, and white miner’s lettuce. After a particularly hard winter we were grateful to see these bursts of color.
This trail passes through Bureau of Land Management (BLM), Crooked River National Grassland, and Oregon Department of Fish and Wildlife land. There is no fee to use the trail and there’s a good parking area at the trail head.
Directions to Otter Bench Trailhead from Highway 97 From Highway 97, just north of Terrebonne, turn left on to Lower Bridge Road (Sign with left arrow says “Crooked River Ranch”). After 2 miles turn right on 43rd St. After 1.7 miles turn left on Chinook Dr. After 5 miles (including a steep descent), go straight on to Horny Hollow Rd (do not take Chinook back up the switchback) Go 1.7 miles to the end of the pavement and park there.
Being a visual person, I have always wanted to visit Bryce Canyon National Park. I was not disappointed when I visited the park in May. Here are some of the many multi-layered delicate castles of stone in the park. They are a visual treat to all that are lucky enough to see them.
Do you enjoy watching the HBO series Westworld? When I first watched the show, I wondered where some of the stunning outdoor shots had been filmed. Interesting land features and sunny skies serve as a backdrop in this series. I found out that several filming locations were in Utah so we visited them on a recent trip.
Origins of Westworld
This series is based on the 1973 Westworld movie, written and directed by Michael Crichton. In this sci-fi classic, wealthy tourists visit an Old West-themed amusement park where they can indulge in any of their fantasies with no consequences. The “hosts” in the park appear to be human but they are actually androids. Though the skies appear to always be sunny, there are dark plot twists involving the hosts in both the movie and the series.
Jonathan Nolan and Lisa Joy worked on the screenplay for the new series. It debuted on HBO in October of 2016. You may have heard of Jonathan’s brother, Christopher Nolan. The two of them co-wrote the screenplays for The Dark Knight, The Dark Knight Rises, and several other successful films. Jonathan worked as a writer, director, and executive producer on the Westworld series, roles he also held for the Person of Interest series.
We just got back from the Rock, Gem, and Mineral Show in Madras. I overheard someone say there were 135 vendors this year so it took a while to see everything. This is the 68th year of this event. It is sponsored by the The All Rockhounds Pow-wow Club of America, Inc. Prices for the rocks, gems, and minerals range from one dollar to hundreds of dollars. Parking, admission, and entertainment is free. The show takes place June 22-25.
Here are a few pictures I took today at the Rock Show in Madras. Do I know what the name is of everything I show in these pictures? No! I have always liked pretty rocks even if I don’t know what they are. If you go to a big rock show like this, someone there can likely identify what’s there for you and tell you all about them. They may even tell a tale or two about the adventure they had when collecting them.
Land forms of the Moenkopi Formation at Capitol Reef National Park, Utah
Land forms at Capitol Reef National Park
The landscape at Capitol Reef National Park tells many stories in colorful layers of rock. The darker columns in the picture above are part of the Moenkopi Formation and it is 225 million years old.
The sedimentary layers of rock in this picture consist of silt, sand, clay, and gravel. The bands of gray and burgundy are made up of volcanic ash. The 700 foot thick layer at the base of the cliffs is the Chinle Formation. That formation contains a lot of petrified wood.
I was impressed by contrasting colors and textures at this park. If you take a trip to Utah, don’t overlook this park. There are a lot of hiking trails here and a short scenic drive.