The Colorado Plateau Part Two

 

Colorado Plateau Country

Colorado Plateau Country

There is a lot of beautiful country on the Colorado Plateau, but there is the other side.  The term many use is the stinking desert.  My home town has an annual rainfall of about eight inches.  Before the Utes were run out and ditches were dug, the Grand Valley was a sparse desert.  The irrigation projects made much of the valley green, but north of the Highline Canal is the desert.  It is a fairly barren desert, not like the Sonoran Desert with its green saguaro cactus.

Mancos Shale Soil

Mancos Shale Soil

The soil, if you can call it that, is fairly infertile, high in salts, and high in toxic selenium.  It’s called the Mancos Shale.  The Mancos Shale, called the Pierre Shale east of the Rockies, runs from South Dakota to central Utah.  It is an ancient sea floor, Cretaceous in age, of the inland sea covering much of North America.  Shale is mud rock, laid down as the sea advanced and retreated over millions of years.

The lower part of the Bookcliffs and the valley floors are Mancos Shale.  In its natural state it is a scrub grassland, supporting small populations of deer, antelope, prairie dogs, sage grouse, cottontails, and some Bison.  When the Northern European Americans arrived, they saw grazing land.  The sheep and cattle came.  The ranchers did well for a few years, but their expectations were unrealistic for such a dry area.  Soon, most of the good grass was gone, replaced by cheat grass and sagebrush.

The area between Delta and Grand Junction is a prime example.  My father, born in 1903, lived in Grand Junction after 1918.  He told me that at that time, there were extensive stands of tall bunch grasses.  They are gone.  That desert is one of the most barren stretches I am aware of.  It is hilly, so irrigation water went to flatter areas.  It is close to towns, so lots of ranchers grazed their stock on the land.

Much of the Mancos shale country is BLM land today.  In the old days, the Land Office and the Grazing Service leased land to ranchers.  There were allocations on the number of head allowed on each segment, but there was little enforcement.  The grass mostly disappeared.  Thus, the stinking desert.

I-70 from Palisade to the west of Green River, Utah is on the Mancos.  Highway Six from where I-70 veers south almost all the way to Price is on the Mancos.  Travelers on those highways have the bare Bookcliffs and the bare desert floor to look at for over 200 miles.  Their impression was what tended to keep the canyon country to the south relatively isolated.  Locals had all that magnificent country mostly to themselves.

Art in Salt Creek Canyon

Art in Salt Creek Canyon

The a uranium and oil and gas booms of the 1950s built a large network of roads and opened the canyon country up for tourism.  Those flat deserts remain empty, along with the mostly shale country of the Bookcliffs and the Tavaputs Plateau to the North.

When I went to Arches in the 1950s, we drove down two tracks winding through the sand.  This year during the height of the season, cars were lined up literally for miles.  Canyonlands National Park is also crowded, people lined up.  I remember going there and often seeing no one.

From Green River to Hanksville is mostly flat, dry desert, with 70 miles from the highway turnoff to the Maze District Ranger Station in Canyonlands.  The greater part of Navajo country in southern Utah, New Mexico, and Arizona is fairly flat desert.  Monument Valley is flat desert that happens to have some rocks sticking up.  Have you ever driven from Albuquerque to Flagstaff on I-40?  Flat desert.

Henry Mountains

Henry Mountains

The Colorado Plateau does have some other features.  Mountains, tall, green, and wet, supplying water to the desert.  Three ranges of mountains, the La Sals near Moab, the Abajos, known to locals as the Blues, and the Henry Mountains, near to nowhere.  The La Sals are the tallest, over 12,000 feet.  The Abajos and the Henrys stretch to 11,000 feet.  They stand in contrast to the red rock country surrounding them, and provide a welcome relief.  People go there in summer to cool off and enjoy the wildlife.

Geologically, the mountains are Laccoliths, formed by a neck of molten magma rising to a weaker junction between two layers of sandstone.  At that junction the magma moves laterally, forming a mushroom shaped dome of igneous rock in the domain of sandstone.  The overlying strata usually erode away, leaving the igneous core.  The Henrys are the type location for Laccoliths, being the subjects of the earliest study, and displaying the domed shape.

Salt Creek Canyon

Salt Creek Canyon

The three ranges are important to ranching, providing water, hay farming, and a summer range, with the stock wintering on the desert.  Salt Creek, draining north from the Blues, has a canyon with year-round water, arches, and Ancestral Puebloan ruins and rock art. The canyon also provides access to a park in the midst of the Needles District of Canyonlands.  I like that park because it was never grazed.  It provides a look at the land before cattle came, trampling or eating everything, mangling stream banks, and bringing alien species like cheat grass.  No I won’t tell you where it is.  Go look for yourself.

 

The Colorado Plateau Part One

Colorado Plateau Scenery

Colorado Plateau Scenery

I am a child of the Colorado Plateau.  I was born and grew up in Fruita, Colorado, and still think of Fruita as home, although I have lived along the Front Range of Colorado most of my life.  The Grand Valley of the Colorado River is near the Grand Hogback, the eastern extent of the plateau in that area.  The Grand Valley is green due to irrigation, but the annual precipitation averages around eight inches a La year, fairly typical of the Plateau.

I am sure that the center of the universe (well, my universe) is somewhere within 100 miles from the confluence of the Green and Colorado rivers.  It is fitting, therefore that the Plateau is somewhat unique geologically.  All those striking layers of varicolored rock formed into spectacular scenery by the work of the Colorado River and its tributaries are relatively undisturbed compared to the Plateau’s neighbors, the Rocky Mountains,  the Basin and Range, the Wasatch and Uintah mountains and the  Mogollan Rim in Arizona.   Pretty neat neighbors, eh?

Those places have been folded, faulted, stretched lifted, collapsed, and otherwise deformed.  The Plateau, on the other hand has remained relatively stable through much of geologic time.  It is this big slab, poked, lifted, twisted, drowned, buried, and eroded several times but still mostly intact.  There were just enough deformation and intrusion to make things interesting.

The reasons for this stability are still somewhat controversial, bit have to do with the Pacific Plate coming our way and north at about the rate your fingernails grow, and the North American Plate headed west at about the same speed.  At different times they have behaved in different ways that, coupled with the somewhat thicker crust under the Plateau, have resulted in this unique region.  I don’t have the space or understanding to explain all those processes, but we can see the result.

An interesting fact is that the entire plateau seems to be rotating clockwise as the Pacific Plate grinds along northward.  That movement is also what is pulling the Basin and Range province apart.  Don’t look for any big changes next week.  This process is really slow.  While all this plate movement is going on, our friends the Green and Colorado rivers just keep digging.  On rare occasions you can see the digging, when there are exceptionally big thunderstorms during the summer monsoon.  A lot of stuff goes into the rivers then.  Today, Lake Powell is catching it, and will become one huge mud flat until the dam eventually fails.

Looking at all these processes requires a different sense of time than how we live from day to day.  In geologic terms, sixty million years (60ma) is relatively brief.  We think of our world as stable (unless you live in the Bay Area) but in truth, everything is on the move, it is just a bit slow.

Upheaval Dome

Upheaval Dome

The Colorado River will eventually bring the entire plateau down to sea level.  Look at Grand Canyon or any of the tributary canyons to see how it works.  My favorite is the San Juan.  Some fine canyons and not as cluttered up with people.  Another place to see the processes of change is Upheaval Dome in Canyonlands National park.  A great big rock came along and smashed down, forming a huge crater and shaking everything up for a long way around.  You can see rocks turned to waves from that hit all the way to Dewey Bridge.

That big crater tried to form a lake, but it is dry there.  The water did make its way to the river, cutting as it went, and now the crater has an outlet.  The crater will get bigger as the cliffs erode back until it is just a depression, then, gone.

There is a plug of gypsum in the crater.  When all that rock was blown out by the impact, the pressure on the stuff under the crater was lowered.  Some of that stuff down there is salt, known as the Paradox Formation, which can flow.  The salt goes into the river, but gypsum isn’t quite as soluble and there it is.  The salt is from an ancient sea that alternated between filling and drying up as sea level rose and fell.  That left a lot of salt which was then buried under a lot of rock.

The Dolores River Leaving the Paradox Valley

The Dolores River Leaving the Paradox Valley

That salt moving around and being dissolved is responsible for much of the scenery in the Moab and surrounding areas.  As it dissolves, some of the overlying rock drops down, creating some fairly large valleys.  Paradox Valley, Sinbad Valley, Lisbon Valley (uranium, oil, and gas), Spanish Valley (Moab), Castle Valley, Fisher Valley, are all big grabens.  They are big blocks that dropped down as the salt leached away. Paradox Valley and Spanish Valley have rivers coming out of a canyon on one side, and going across the valley into a canyon on the other side.  Moab has the Colorado, Paradox has the Dolores.  That makes for some fine scenery.

Paradox Salt Disrupting Things

Paradox Salt Disrupting Things

The fins and arches in Arches and Canyonlands come from the same process on a smaller scale.  All that magnificent scenery is a result of that ancient sea floor full of salt being buried by a colorful succession of rocks that the rivers and the wind could work on.

An exception to the salt influencing the process resulting in fins and arches is Rattlesnake Canyon in Colorado near Fruita.  The river is solely responsible for the work.  The arches are just as cool, and not all full of people.

Next time, some of the other interesting things about the Colorado Plateau, one of the most interesting places on the planet.

The Broadmoor

 

The Broadmoor

The Broadmoor

Recently we were at the Broadmoor Hotel in Colorado Springs for a family celebration.  I used to live in the Springs and we would go there for dinner or a Colorado College hockey game at the old World Arena.  I saw some world class figure skating there as well.  Over 20 years ago we were there for the Christmas package deal.  A room, show, and dinner for a good price.

Back then, the Broadmoor was five star, but beginning to get a bit frayed around the edges.  It is not frayed now.  Millions have been spent on renovations, a new golf club, the Broadmoor West hotel, amazing landscaping, new restaurants, attentive and helpful service, and a host of other amenities.  The old World Arena is gone, but the Broadmoor now owns the new World Arena about five minutes from the hotel.  There is a new golf course, a big back country lodge, and bird shooting along the South Platte River.

Great Beds

Great Beds

The Penrose Room, the formal dining room, the Golden Bee pub, and the Taverna remain for the traditionalists.  One of my guidelines for assessing a facility is the attitude of the staff.  The Broadmoor is five star.  The staff is trained to be friendly with guests, but their attitudes seemed genuine.  I think they like their jobs.

The setting is outstanding as well.  Cheyenne Mountain is the backdrop and in this wet summer is just beautiful.  The neighborhood is beautiful as well, upscale homes with mature manicured landscaping.  Colorado Springs is a fine city, with that mountain looking down on everything.

Room rates are somewhere from $300 per night up, with charges for everything.  It costs $24.00 per night to park your car.  Entrees in the dining rooms start at $15.00 and go up.  Way up.  The food is excellent, although I had a fennel dish that did not measure up.  There was also some confusion with our room reservations which should not have happened.  The bed in our elegant room was the best I have slept in.

broadmoor4We had dinner in the Italian Restaurant in the west hotel.  We were lucky to have perfect weather, and the dining room opened up to the lake that was staggering in its beauty.  Truly a world class setting for a world class resort.  We had drinks on the patio at sundown and listened to the bagpipes.

The Broadmoor’s history is connected with the Pikes Peak region history.  The gold from Cripple Creek made Spencer Penrose’s fortune, and mouth of it went into the hotel. A few men made a lot of money from the mines, and a lot of it went into making Colorado Springs a lovely city (at least the older parts).

A lot of that history is depicted in the photographs and art in the hotels.  The hotel also has a good collection of Western art.  For example there is a painting from the 1840’s that depicts a wagon train just ready to go on the trail.  For this history buff, I learned some things from that painting. The bronze sculptures range from famous Fredrick Remingtons to romantic kitsch, typical of western art in general.  There is a fascinating display of wine and liquor bottles dating from the  prohibition era.  It seems that if you were rich enough, the rules didn’t apply.

I have stayed at the Brown Palace and the Ritz-Carlton at Half Moon Bay.  I prefer the Broadmoor.  I think we will have to go back at least once.

 

 

Small Towns

Paonia

Paonia

I am a city boy now.  After leaving Fruita to go to college in Boulder, I have mostly lived in cities.  I like the culture, the business, and the amenities that come with the city.  Here I am in the coffee shop right nest to the Denver University campus, with the energy those young people bring.  It helps my writing.

I grew up in a small town, and they still exert a pull on me.  I spent a couple of summers in Keystone, South Dakota peddling turquoise jewelry to the tourists.  I got to know some of the locals during that brief time and enjoyed the Black Hills culture.  I get back to Fruita some, my 55th reunion is coming up, and like rekindling old friendships.

Last weekend I made a quick trip to Grand Junction and Fruita on family business.  There are a lot of memories there, and I enjoyed the feel of a much larger town than it was all those years ago.  Bad news: the pool halls are gone.  Good news:  you don’t have to settle for chicken fried steak in the restaurant.

 

After my adventure in Rattlesnake Canyon the day before, I decided to take a scenic route back to Denver.  My first stop was Collbran, a town on Plateau Creek I have always liked.  I was looking for the landslide that killed three men last spring, but went up the wrong creek (story of my life).  At the gas station, a local rancher and his son had their rubber boots, so we talked about irrigating for a while.

I went over Grand Mesa and drove through Cedaredge, another favorite small town.  I like Cedaredge for the view of the Uncompahgre Valley, the Uncompahgre Plateau,and the San Juans.  No view last Sunday, the smoke from all the fires in the northwest obscuring everything.  Cedaredge and Eckert right down the road are nice towns, but the highway runs right through town, as it does in Collbran.  The roads are noisy, busy, and sort of split the town.

I had lunch in Paonia, just about my all-time favorite town but for the fact that they usually killed us in football.  My senior year we lost so badly that I even got to play.  Paonia is off the highway and is the home of High Country News, a great magazine about the west.  The West Elk Mountains are just out of town, but the area’s economy is mostly farming and ranching.  They grow peaches, cherries, apples, and lately, wine grapes.  They have a nice mild climate right at the foot of the mountains.

I had a good hamburger in one of the restaurants and drove around a bit (that takes about fifteen minutes).  I was struck by the life in the town.  OnSunday morning families were out walking and kids from age six on up were riding their bikes all over town.  The last town I remember seeing that was Winslow, Arizona.

So, my main criteria for a good small town are no McDonalds, no Walmart, a farming economy, and school age kids on bicycles.  I don’t think I will ever leave the city, but if I do, it will be to a town like Paonia.

Rattlesnake Canyon

Dramatic

Dramatic

Rattlesnake Canyon is near Fruita, Colorado, where I grew up.  My friends and I  ran all over the hills north and west of the Colorado National Monument, but I had never been to

Rattlesnake Canyon.  It is a bit too far for kids on foot.  We got into the canyons just east of the canyon, now part of the Black Ridge Wilderness, but I did not know about the arches in Rattlesnake Canyon.

Close to town, the canyon is a bit tough to get to.  The Pollock Canyon trailhead near the river means an overnight backpack to do justice to the country.  The other route follows Black Ridge west from the Glade Park Store, and is for 4×4 vehicles or Subarus you are willing to bash around.  From the trailhead it is about four miles on the trail if you take the shortcut.

I have rambled around the Colorado Plateau off and on all my life.  From the Grand Canyon to Dinosaur and from the Grand Hogback to the Wasatch, the plateau offers some

Rattlesnake Canyon

Rattlesnake Canyon

of the most magnificent country anywhere.  Rattlesnake Canyon is up there with the best.  Arches has more arches, and there are bigger canyons (not that many), but Rattlesnake has it all.  The real bonuses are that it is close and not cluttered up with people.  With the exception of Grand Canyon, most anywhere else offered some solitude at one ime.  No longer.  Thirty miles from Grand Junction, with a competent high clearance vehicle you can be in wilderness in view of Fruita.

Ah, the sense of space.  I live in the city and it is impossible to have a sense of space, even with Mt. Evans looking down at you.  From those canyon rims the expanse opens my mind.  Grand Mesa, the Bookcliffs, and the Roan Cliffs rim the Grand Valley, quite a scene by itself.

The canyon walls are Wingate sandstone capped by harder Kayenta sandstone.  That cap rock forms a bench with the Entrada sandstone (slickrock) set back from the rim.  Rim Rock Drive in the Monument is mostly on that bench, and the trail to Rattlesnake drops down on the bench and curves around the canyon rim to the arches.  The arches are in the slickrock, ancient sand dunes turned to stone.  It is easy to see the rounded dunes in the rock.  Erosion works its way into the cliffs following the curve of the dunes, forming alcoves.  As the alcoves erode farther, sometimes the back of the alcove drops out, leaving an arch.  I saw six of them. Arches in Colorado, the second largest concentration in the country, maybe the world.

About that trail.  I got away from Denver at 6:00 AM, not my best time of day.  I filled my water bottle and left it on the kitchen counter.  I didn’t realize it until I was at the trailhead at about 1:30 PM.  I am also out of shape, my exercise restricted by a couple of broken ribs for five weeks.  Have I mentioned that I am 72 years old and impulsive?  I looked at the sign, 3 1/2 miles.  It was only 90 degrees or so, a piece of cake.

First Arch. Where I climbed up the rock through the arch.

First Arch. Where I climbed up the rock through the arch.

I covered about half of the trail when I realized I was getting a bit dry.  “Keep going, I can drink later”.  The arches were a progression along the bench and close to the trail.  With that row of arches on one side and that magnificent canyon with 400 foot sheer walls branching into side canyons on the other side, I was literally staggered by the beauty.   Well maybe the stagger was because I was tired and thirsty.  I caught up to a party of six people at the last arch, known as First Arch.  At First Arch was the sign saying End of Trail.  I didn’t know that, and by that time I was stopping to rest fairly often, so while resting I watched the party climb up the slickrock through the arch.  I knew the trailhead was only about 1/2 mile from the arch.  So, it was climb up the rock through that impressive arch or backtrack 3 1/2 miles.  I climbed.

I have done a lot of sandstone climbing, and used to be pretty good at it.  That was when I wasn’t 72, tired, getting sore, and thirsty.  I climbed anyway.  I would do about 20 feet, catch my breath, figure out my next moves, and climb again.  The proper way to climb that stuff is on your feet even if it is steep.  Feet have more traction than denim, and the work is easier than trying to slither up.  I slithered.  I was too weak to trust myself trying to walk up those steep slopes.

The rock has curves, little depressions, some tiny ridges, notches, and hollows to give one a way up.  I tried to pick the easiest route, but it was still pretty steep.  My knees paid the price, getting some good scrapes.  Up on the rim, that last half mile was tough.  It was uphill, but not too bad.  I stopped twice and flopped down in the shade for a few minutes while walking slowly back to the truck.

There was about 1/4 of a cup of coffee in the truck that sure tasted good.  I was lightheaded and pretty wobbly during the drive out.  I stopped at the Visitor Center in the Park and drank water for a while.  I got a motel room in Fruita about 6:00 PM, didn’t eat dinner, and drank water until lights out about 9:30.

Sunday morning I had breakfast, drank water, and took the scenic route back to Denver.  I drank water and went up Plateau Creek to Collbran, went over Grand Mesa to Paonia where I had lunch and drank water, then over McClure Pass to Glenwood and home on I-70.  I was fully rehydrated by Monday.

I didn't see a rattlesnake in Rattlesnake Canyon

I didn’t see a rattlesnake in Rattlesnake Canyon

After a few minor incidents in the backcountry over the years, I have developed several rules to follow when Out There.  Take water.  Take enough water for the other persons you come across who didn’t bring enough water.  Be in shape.  Research where you are going so you know what to expect.  Have a map. Carry the ten essentials in case you get into trouble.  Tell people where you are going.  You really should not go alone.  I broke every rule.

What the fuck is wrong with me?  I know.  I am an impulsive ADD.  When I got to the trailhead and saw I had no water I should have driven out.  But, I wouldn’t have this story to tell.  What I did do right was pace myself, not panic, and take my time getting out.  It is just that my brain didn’t kick in until three hours too late.

 

The Not So Lost Summer

 

grumpyIt is mid-August and I have not been out of town. How is that for a rambling Colorado native? My broken ribs are healing, Carol’s complicated cataract removal is slowly healing. Neither one of us is supposed to lift, I can’t bounce four wheeling, and Carol is not supposed to bend over. Life under those conditions is a bit difficult. So, no traveling.

Frustration sums up my mood. The frustration has slipped into irritability, insomnia, and advanced cabin fever. Life is not entirely wasted, however. Reading is difficult for Carol, so I have read six novels aloud. I enjoy that,and so does Carol. We have seen some movies, mostly bad, and I am at the point where I can follow the plot lines of her TV programs.

This week I put up a post on www.dofbill.com about the Bookcliffs in western Colorado and eastern Utah. Writing the post required me to do a lot of reading about Colorado Plateau geology, maybe my first love. Growing up in Fruita and wondering how that elevated horizon in every direction got there inspired the seeker in me to learn why? I am still learning.

So, you are going to get more geology to read about if you can stand it. Don’t worry, I will only go back about 1.8 billion years.   From the Grand Canyon to Vernal, Utah is a mostly complete record in stone (and mud) of American geologic history.

The summer hasn’t been lost, but I sure do have the itch to go WEST. I may also be flying to New York and driving a car back. I love solo road trips. Time to think, see, and eat bad food. Carol’s daughter is hitting the big five oh, and there is a celebration at the Broadmoor coming up. I am also trying to decide if I am going to my 55th high school reunion during the Fruita Harvest Festival. It should be fun, but I have had too many reminders about how old I am this year.

After putting that limited slip differential in my Toyota, I have been on one four wheeling short drive and didn’t get a chance to try it out on the fairly good roads. The Bookcliffs area is mostly shale that turns to the slickest mud in North America when wet. I can’t wait.

I have a crossover tool box in the bed of the Toy that is filled with recovery gear. Two sets of tire chains, tow chain, tow strap, come-along, shovel axe, saw, high-lift jack,tools, and enough stuff to keep me alive if I end up stuck somewhere. All that stuff is so heavy it has damaged the aluminum toolbox. I have propped it up with a couple of 4x4s until I can lift all that stuff out and get the toolbox replaced. No lifting, remember? I’m glad the toolbox has a lifetime warranty. I wish I did.

Happy

Happy

Life is OK. The cabin fever with a sore back has brought me down more than it should have. The Buddhists make a distinction between pain and suffering. I let the pain of an injury go into suffering. While I was suffering, life was really pretty good. It’s all about how you look at it, and I was looking at the dark side.

The Bookcliffs and the River

 

Bookcliffs

Bookcliffs

The Book Cliffs are the neglected stepchildren of Western Colorado and Eastern Utah. That is somewhat ironic, because they stretch from Palisade and Mt. Garfield about 200 miles to Price, Utah. Rising about 1000 feet from the valley floor, they are the longest escarpment in the world. Above the Book Cliffs is a bench With the Roan Cliffs forming another escarpment  Behind the cliffs is the Roan Plateau, rising to about 8000 feet in elevation. With the wide change in elevation and precipitation from eight inches annually to around thirty, there is wide diversity in plant and animal life. There are energy resources as well. Natural gas, tar sands, oil, coal, and that huge deposit of oil shale.   The region is known as the Tavaputs Plateau.

The plateau is home to the Desolation Canyon Wilderness and due to the wide range in elevation and precipitation, a diverse range of plant and animal life. There are three reasons why the area is not very popular with visitors.

First, look south. Colorado National Monument, Arches, Canyonlands, Capitol Reef, Bryce Canyon, Zion, and Grand Canyon National Parks. There are the three mountain ranges and all that wondrous red rock carved into some of the best scenery on earth.

Next, accessibility. Douglas Pass is the only paved road in the vast area. The many dirt roads are accessible only as long as they are dry. Traditionally, the only people there were stockmen and the Utes on their reservation. In recent times there has been much energy-related activity that comes and goes.

The third reason? Shale. It is not only shale, there are layers of sandstone, even limestone. It’s all gray or shades of tan. Driving on the drab Mancos shale landscape of I-70, looking north you see drab cliffs. More of the same gray rock, just standing up. Roads built on that shale changes into some of the most slippery substances known after a rain or snow.. People are just not inspired to go there.

Growing up in Fruita, Colorado, I spent quite a bit of time in areas on either side of the Douglas Pass road, which was gravel and dust at the time. We had rancher friends, and deer season was a big social scene. It is wild, mostly empty country, home to lots of cattle, some sheep, a few ranchers, and a lot of wildlife. It is also famous for some of the most treacherous mud in the world. There are some sandstone lenses (we called them rims), but it is mostly shale, a former lake bottom that now sits thousands of feet above the Grand Valley, where the people live.

Colorado National Monument.  Bookcliffs on the horizon

Colorado National Monument. Bookcliffs on the horizon

I used to look at the Colorado National Monument with its red rocks to the south. To the north were the relatively drab Bookcliffs with the whitish Roan Plateau above them. Why the difference? The Monument is famous, with lots of information about the Uncompaghre Uplift lifting the Uncompahgre Plateau thousands of feet compared to the Grand Valley. As the plateau, erosion took the more recent rocks off, leaving the more resistant sandstone.

I thought some sort of uplift must have formed the Bookcliffs. Well, partly. When the entire Colorado Plateau was uplifted at the same time as the Rockies, The Colorado River just dug away, carrying the eroded rock to the sea. It is still digging, and is eroding those Bookcliffs to the north. Under the Bookcliffs are the rocks of the Monument. Someday the land will be fairly flat between Grand Junction and Craig. We won’t be around, however. These things take time.

So, the Colorado Plateau was uplifted and after that the Uncompahgre Plateau went up some more and wore down. The rocks exposed at the Monument are, a few miles north, well below the rocks of the Bookcliffs who are headed north as the river gnaws away. The Colorado River rules, it is just a bit slow.

Changes

 

I am a slow learner, especially when I don’t want to learn what the universe is trying to get across. For some time now, the message is to slow down and act my age. I don’t want to! I want to be younger, stronger, not forgetful, with no signs of aging (well, I’m resigned to being bald).

broken-ribsWell guess what, I’m old, slow, weak, with a bit of a balance problem. In the last couple months I have fallen twice, fell off the ladder, and fell down the last step and broke two ribs. As I mentioned, I’m a slow learner. It’s shocking, I know, but I am going on seventy three years old. After the first two falls I saw my doctor. She gave me a prescription for physical therapy to help my balance. I didn’t go. I then fell off the ladder and down the stairs. Did you know that broken ribs hurt a lot?

After the ribs broke I went into a blue funk. At that point I had no choice. I hurt and couldn’t do anything but read. I can barely stand to watch TV. Then, horror, my iPad died. No Facebook, no words with friends, no left-wing politics, and no Donald Trump news.

Apple Rules! The Apple Store is in Cherry Creek Mall. The Apple Store is full of people, the rest of the mall is virtually empty except for the mall walkers. After the standard long wait I made it to the Genius Bar. The sheer arrogance of that company! The guy was nice and gave the standard digital solution. Reload the operating system, wiping all my data.   Oops, that didn’t work, hardware problem. I walk out of the store with a new iPad.

Most everything transferred over. But. I can’t get to one of my email accounts, Yahoo is unresponsive, I am starting over with Words With Friends, and two days are gone. Computers teach us how to deal with frustration. To a point. I didn’t use the iPad as a Frisbee. The upside? Apple is a bit richer and the process took me off my aging crisis.

The odd thing about aging is that I still feel like me. The same me. Not a old me, just me. But, the body doesn’t feel the same. Even the mind has changed. I forget stuff. I have never been a good rememberer, but I’m worse now. The me I used to be never fell down the stairs. I fell , but not too often, just more than you do. Now I fall a lot more than you.

I know how to fall. Tuck and roll, keep the head up, pick a good spot to land if you can. The skills have served me well. Only two bad ones, one on the motorcycle that finished off my bad knee, and this stair and rib thing. Well, except for the fall that ended up taking my right little finger. For some reason, the universe has chosen falling to convince me that I am no longer the guy I used to be.

A Facebook Friend asked me if there was more damage than the broken ribs. My response: Yes.   I am forced to accept that I am changed. Older. Slower. Weaker. Unbalanced (Wait, that’s always been true.), just not as physically competent as I used to be. A lot of bad stuff is going on. I am not even going to go into the health issues.

I’ve had good changes in recent years. I got my ADD diagnosed and got the medication and cognitive therapy that has changed my life. Just the diagnosis was a big deal. I am no longer a guy with a fatal flaw. I am a guy with ADD. It’s a brain disorder, not just that I am a fuckup.

The biggest change is that with the ADD treatment I now have the focus to write. Other than falling in love and marrying Carol, that is the most profound change in my life. I have two callings, writing and teaching. ADD kept me from both pursuits. Now, however I can write. I may be an old guy, but after all these years I have enough focus to write. After the rib thing I couldn’t write for a while-pain, both physical and mental.

Both kinds of pain are better now. I guess my old guy crisis is not as bad as I thought. The Buddhists say that pain is inevitable but suffering is optional, a choice. For a couple of weeks I suffered. Now my ribs just hurt, but they are feeling better every day. It is mostly over.  I guess it is time to get on with life.

Backpacking

Backpackers

Backpackers

Back in the 1970’s and 1980’s I did a fair amount of backpacking.  I have stumbled around in mountains, up 14000 foot mountains, in the heat of desert summer, and in winter.  I suffered, limped, ate bad food, and drank bad water.  There was joy, serenity, fear, and awe. I can’t backpack now, old and with knee and back problems.  The memories of those trips will be with me always.  There is more satisfaction in accomplishing something that took a lot of work.  The most work was carrying a loaded pack up Mount Princeton and slogging through two feet of fresh spring snow in Loch Vale, Rocky Mountain National Park. Those winter backpacks have additional challenges.  It is dark for a long time and it is cold out there.  The bladder just does not respect any difficulties in getting it drained.  How long can you lay there before struggling out of that warm sleeping bag, covering the feet, donning a coat, and stumbling outside.

Loch Vale

Loch Vale

In Loch Vale it snowed a lot of heavy wet snow.  We knocked snow off the tent and listened to the snow slides run.  We had made camp in the dark and didn’t know if we were in a slide area or not.  I guess we weren’t.  It was still snowing without much visibility when we headed for the car.  We made a wrong turn and went down a steep gulch.  Have you ever tried to sidehill in two feet of fresh snow, hardpack underneath, with snowshoes?  At one point I just flopped down in the snow and laid there for a while.

Fiery Furnace

Fiery Furnace

The best winter trip was in the Fiery Furnace, Arches National Park, in February.  Clear weather, no snow, and no one else there.  If you haven’t been to the fiery furnace, go.  There are hoops to jump through with the Park Service these days but it is worth it.  Don’t go in summer.  Another good trip on snowshoes was a spring trip on Grand Mesa.  Longer days, no one around, but the snowmobiles had made a packed trail for us.

North Park is a big, mostly empty place where the North Platte starts its journey north.  The east side has the Rawah Wilderness, while the south rim has the Mt. Zirkle Wilderness.  The Zirkle trip was a lot of fun with good people, but the Rawah trip was something of an adventure. We went with another couple for a several day trip, starting from the Laramie River road north of Cameron Pass.  My wife at the time and I had gained some backpacking experience and were fairly confident in the boonies.

Rawahs

Rawahs

One of the other couple had gone to the National Outdoor Leadership School in Lander.  She was not just a convert to the NOLS way, she was an evangelist. NOLS is a highly respected organization, but Paul Petzolt, the founder had strong opinions about wilderness behavior and equipment.  Most of his ideas have become mainstream, such as Leave No Trace.  His ideas about equipment, however, were a bit old-fashioned (He was in the 10th Mountain Division in WWII.). The equipment was good, but heavier than what people were using thirty years later.

We met several times with them to plan the trip and make up meals.  Most of the food was light weight, but from the grocery store, not the freeze dried stuff.  It meant a lot of measuring, mixing, and packaging.  One of the lunch items was what was a precursor of Power Bars.  Peanut butter, fruit and nuts, oatmeal, and other stuff I don’t remember.  We rolled them into cylinders that looked exactly like turds.  They didn’t taste like that, but I have never had them since.  I think they were a NOLS idea. The other part of those meetings was listening to NOLS stories, and how the school made the graduates wilderness experts.  We heard a lot of stories.  I shudder every time I am near Lander.

Almost all backpacks in Colorado start with a climb.  We started at roughly 8000 feet elevation and made camp just below timberline, which is usually around 11000 feet high.  A good hard climb with a pack on your back.  We made camp, and our NOLS wilderness expert went right to bed with altitude sickness.  She was fine the next morning, and we heard no more about NOLS.  Sometimes altitude sickness can be a blessing.

Here it Comes

Here it Comes

The Rawahs are a long ridge with several peaks in the 12000 feet range.  One day we climbed to the top of the ridge.  A fine view, with North Park below, and the mountains of the Continental Divide to the south, and with the Zirkle across the park. We didn’t stay long.  A huge thunderstorm was headed our way across North Park.  We left in a hurry.  We didn’t make it to timberline before the storm hit.  If you want to experience terror, be in a lightning storm with no place to hide.  Lightning was striking all around us and the noise, with nothing but rock to reflect the sound from the crashes.  The wisdom is to crouch down in a bit of a low spot.  We ran.  I guess we made it. Another time I will write about desert trips.  My favorite part of the world is the Colorado Plateau, probably because I was born there. The two most memorable experiences of all were snow in Loch Vale and lightning in the Rawahs.

Motorcycles

Kawasaki KLR 650

Kawasaki KLR 650

I have owned and ridden three motorcycles.  I like motorcycles. They are as close to flying as one can get on land.  There are challenges, such as trying to stay upright on two wheels. I know people who have never been down on their bikes.  I once fell over right by the front door of the biggest motorcycle accessory shop in Denver.  It trapped my leg and some guy had to lift it off me.  I bet he is still telling that story.

I have crashed on city streets, on a paved canyon road (sand), in parking lots, and an uncountable number of times in the dirt.  Two of my motorcycles were what is now called dual sport; they are able to be used on the street and in the dirt.  They aren’t top notch in either role, but some riders do things most people can’t imagine.  80 mph on the highway, and some challenging back country roads and trails.  Lots of good dual sport roads in Colorado, Utah, New Mexico, and Wyoming, where I traveled.

One of the best grew up riding on the streets of Mexico City, where you have to be good to survive.  I could keep up with him on the highway because we had the same bikes.  In the dirt, he could go places with that fairly heavy thing that I didn’t even dream of.  He and quite a few others have done 50 mountain passes in Colorado in 50 hours.  I am good for about six in a day, and hurt for two days. He also did a lot of single track trails, something I never attempted.

I liked road trips with some gravel or dirt roads thrown in.  Forest Service roads were about as gnarly as I wanted. On the asphalt, it was curves in canyons.  Fortunately, Colorado’s Front Range has lots of canyons.  There was a geological event that bumped the long bench from Conifer to its Estes Park.  That bench was once at Denver’s elevation, but got pooched up to where it is now.  We call the road the Peak to Peak Highway.

Golden Gate Canyon

Golden Gate Canyon

Go up any of the canyons from Deer Creek to the Big Thompson, ride those fast sweeping curves a ways, then down another canyon.  My favorite was Golden Gate Canyon, where I tore my posterior cruciate ligament when I hit some sand on the road.

It’s the lean, folks.  Go around a curve on two wheels and you lean.  Go faster, lean more.  Go faster, and crash.  I went fairly slow for a motorcyclist.  I still got some lean, and was able to look at the geology.  A low side crash is when the bike slides out from under you and goes off the road ahead of you.

High Side Crash

High Side Crash

A high side crash is the bad one.  The front wheel starts to slide, then gets traction.  You are flipped off and into the air, while the bike bounces along behind until it lands on you.  Both are bad, but you really do not want to high side.  Some riders get flipped into the guardrail.  Ouch.

My knee wrecking crash was a low side.  My knee was bent, the tibia-fibula stopped on the pavement while the femur went a little farther.  It really hurt.  Hurt bad. I picked the bike up and rode on until I couldn’t stand the pain and called for help.

Aside from the crashes, I loved motorcycling.  Yes, it is dangerous.  Other drivers don’t see you and turn in front of you.  You crash all by yourself.  There is a famous twisty road in North Carolina where a biker went into the bushes. Just in front of him was another motorcycle with the remains of the rider.  He went into the bushes and nobody saw a thing.

Yamaha SR 400

Yamaha SR 400

I always wore all the protective gear.  Those Harley riders who won’t wear a helmet because their balls will protect them are nuts.  Mass delusion, those Harley people.

This spring I got the itch again.  Yamaha makes a single cylinder bike that looks a lot like the classic British thumpers from the 1950s.  It isn’t fast, but sure would be a good canyon bike.  Nah.  Too old and slow myself.  I guess I will stick to four wheeling.

 

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