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Our property is a regular herpetarium. We have wall to wall lizards ranging in size from tiny babies that have hit the ground running up to foot-long alligator lizards that can scare the heck out of you. We also have skinks, beautifully iridescent lizards with bright blue tails.
Fence lizards dominate, however. You can’t go outside without seeing dozens at this time of the year. They are fun to watch as they scamper across our yard in search of bugs. And they are even more entertaining when they try to impress another lizard by doing push-ups and puffing up their bodies to almost twice their normal size.
They are also quite curious. Or at least they seem to be. Anytime I am outside working around the house, they show up and watch me, often choosing a high perch for a better view. If I do something that chases them away, they’re back in a minute or two. The fellow below came out to watch me when I was building a brick planter around our yellow rose bush earlier this week.

I think we have seen all of one wren since Peggy and I moved here. But a couple of weeks ago, a pair showed up looking for a home. It was pretty funny. The male wren, it turns out, is responsible for house hunting and nest building. The location may be a tree cavity, a birdhouse, a drain pipe, etc. Even an old shoe will do in a pinch. Once he finds what he considers the ideal site, he fills it with twigs and invites his lady love over to check it out. She’s the one that makes the ultimate decision about his nest finding abilities. I can see where she might be concerned if he has picked an old shoe. The poor guy may find himself building 3 or 4 nests before she finally says yes.
I think ours must have been on number four— or maybe five— when he showed her our bird house. He seemed very eager, or maybe he was nervous, like a real estate agent about to close or lose a big sale. He talked and talked and talked. Finally, she hopped in to take a look. And immediately hopped out with a feather in her mouth that she spit out. I could almost hear the discussion. “You are trying to sell me a used house!” “No, no sweetie. Think of it as an already feathered nest.” Whatever he said, she went back inside and came out with another feather. This time she ate it! Apparently that meant yes because the little guy started hopping around and talking twice as fast. Then he zoomed off to pick up some grass to add to the nest. Soon, they were both busy at work.





I’ll close today with a few more photos of the deer herd. Do you remember when I did the post on young buck and his fearless leaps over a wall and a fence to get at our honeysuckle and native shrub garden? Well, it turns out he isn’t so young…




Tomorrow’s post: Who knows? Not me. (grin)
Peggy and I were sitting in our library downing an English muffin and a bowl of fruit on Friday morning when a movement outside caught my attention. A fox was climbing our eight-foot deer fence after a Stellar jay that was hassling it. Once again we found ourselves in a zoo looking out from our comfortable cage. The fox climbed down, made its way through our shrub garden, and climbed under the fence. I took this photo right after it climbed under the fence.

Given its reddish color, my first thought was red fox, but its black capped grey tail and climbing ability quickly identified it as a grey fox. Grey foxes are the only ones that climbs trees (and apparently deer fences). They have even been known to raise their families in tree dens high above the ground. We catch glimpses of them occasionally on our property but normally they are secretive. One time, we watched a doe stalk one, following along behind, carefully raising and placing each hoof. That was neat.
My guess is that they have a den (or dens) on our property. The male and female raise the kits together. For the first couple of weeks the mother tends to her babies while the male hunts and supplies food. Our experience is that they form a close bond. A few years ago a fox was run over on the highway below our property. Each night we would hear its partner howling down on the road. Only when I went down and buried the fox did the howling end.



Having enjoyed the fox, it was only appropriate that we would see a coyote as well. We met up with it last week as we were hiking in the forest behind our house. It seemed as curious about us as we were about it.


This is hot off the press, and it isn’t about Covid-19. Woohoo! I was skimming through Apple News this morning and I came across an article that bumble bees bite plants. How could I not read the article? Had the plants somehow irritated the bees. Was there a bee-plant war going on? No, there wasn’t a war. The bees depend on the pollen from the plants for their survival. But they were irritated. The plants weren’t blooming and providing the pollen. So the bees bit the plants to speed up the process. Apparently it cuts two to three weeks off the wait period. I rushed outside to see if I could spot a bumble bee biting a plant. No luck, the flowers were already blooming. I did catch a couple of photos of bumble bees harvesting pollen, however. I conclude my post with them. Bzzzzzzz.


NEXT POSTS: Tomorrow I’ll take you window shopping in Venice. Thursday: Part 2 of nature tales. Among other things, you will meet a Buddhist lizard.

Unusual rock formations created by minerals from dripping water led the Oregon Caves to be set aside as a national treasure in the early 1900s.
Claustrophobia: A fear of confined places
Acrophobia came up in my blog about Mt. Whitney. No surprise there, thousands of feet are between the hiker and a rather unfortunate landing. Splat! It’s a reasonable fear. Claustrophobia is just as real as fears go, but more irrational. The odds of being squished in a tight space— unless you are Indiana Jones or a misplaced wookie caught in a starship’s garbage disposal unit— are between slim and none. Don’t sweat it, right?
Try telling that to someone who is claustrophobic. I suggest you don’t stand between her and the exit. I get it. I am not particularly fond of enclosed spaces myself, whether they are physical or mental. I don’t like driving through tunnels and I hate freeway construction where imposing cement barriers shrink down to your vehicle’s width and provide a view of what hell is like. And that’s even before the gigantic truck comes barreling down on you and breathes fire up your tail pipe because you insist on driving 45 MPH in a 45 MPH zone. At least I can take my revenge when they put up plastic cones instead of cement barriers, as Peggy might tell you. Crunch. Curt strikes another blow for freedom.
Where does this leave me with caving, or spelunking, as the sophisticates call it? How do I feel about getting down on my belly and crawling through a space my skinny fourteen-year-old body would have gotten stuck in several hundred feet under ground? Not a problem; it’s not on my to-do list. But for some unfathomable reason, the standard well-known cave tours don’t bother me. In fact, I find them fascinating. Stalactites and stalagmites tickle my fancy and stir my imagination.

These small stalactites show tiny drops of mineral laden water that come down from a tube in the center of the stalactite. They will add about an inch of growth in a thousand years. (Photo by Peggy Mekemson.)

This photo from Oregon Cave National Monument shows the development of stalactites (coming down) and stalagmites (going up). Eventually they meet, as demonstrated on the left. (Photo by Peggy Mekemson.)
So when Peggy suggested we head off to the Oregon Cave National Monument for her birthday a couple of weeks ago, I readily agreed. We’d been talking about it ever since we moved to Oregon. Except for the last few miles of the road that shot up a mountain and redefined the meaning of curves, the hour and a half drive was quite pleasant.
A ranger greeted us and gave us the bad news. We should expect a two-hour wait. He also wanted to know if we had been in any eastern caves in the last five years. If so— no go. White nose syndrome was wiping out eastern bats. So far their western cousins had lucked out. It had been six years since we had visited Mammoth Cave in Kentucky. We were in by a cat’s whisker.
Our wait turned out to be just over an hour. There was barely time for lunch and a look through the visitor’s center before we found ourselves at the cave entrance shivering from a blast of 44˚ F air. “Cave’s breathe,” our guide stated. He also told us about the 500 narrow stairs we would be negotiating and the low ceilings. I would be bent over double with my size 14 shoes balanced precariously on wet slippery rocks. I looked enviously at a small girl who would be standing up straight with her feet resting solidly on the narrow stone steps. She gave me an impish grin.

Dimly lit stone steps make their way up from what is known as Ghost Cave. The narrowest ones were about half the depth of my size 14 shoes. (Photo by Peggy Mekemson.)
The Oregon Caves are somewhat unusual in that they are made out of marble. Once upon a time they were a coral reef far out in the Pacific. Plate tectonics sent the Pacific Plate diving under North America and scraped off portions of the ocean floor some 100 million years ago, adding new land to the continent. The tremendous heat and pressure involved changed the lime into marble. Folding, faulting and water created the caves.

Another example of the impact of lighting. The rock on the left had been signed by all of the members of a geology class that had visited in the 1800s. Strict rules are now in place to protect the cave.

Tour over, Peggy and I stand on top of the mountain that contains the caves. This photo gives a perspective on the surrounding countryside.
NEXT BLOG: Peggy and I are headed off for a brief hiking tour at Mt. Rainier National Park for the next several days so I may be out of computer range. When I come back I will report on my recent experience as a chicken farmer: The Chicken Whisperer.
To say the least, Mono Lake is a strange place. Some people even call it weird. Once upon a time, back when glaciers stretched across North America, it was part of a series of large lakes that covered much of modern-day Eastern California, Nevada and Utah, a region that is now primarily desert. Left behind as a remnant by retreating glaciers, Mono Lake is at least 760,000 years old and could be as old as three million years, making it one of the oldest lakes in North America.
What flows into Mono Lake, stays. There are no outlets. As a result, the lake is 2-3 times as salty as the ocean. Swimmers don’t have to worry about sinking. In fact the lake contains some 280 million tons of dissolved salts, which makes it even too salty for fish. An effort to introduce trout left them belly up on the surface, like the proverbial dead gold-fish destined for a close encounter with the family toilet.
Algae, brine shrimp, and alkali flies thrive in the water, however. The thumbnail-sized shrimp population is estimated to be somewhere between 4 and 6 trillion in the summer. Historically, the fly pupae served as a major source of food for the Kutzadika’a Indians. In fact, the name for the tribe means fly eater.
Today, both the flies and shrimp provide food for some two million birds that migrate through the area. One visitor, Wilson’s Phalarope, a tiny, fist-sized shorebird, takes advantage of the gourmet flies to double its weight and grow a new set of feathers before journeying 3000 miles to South America— a feat that is accomplished in three days of nonstop flying at speeds of over 40 miles per hour.
It isn’t flies, shrimp, birds, or salt water that Mono Lake is famous for, however. It’s tufa, the fantastical, fairy-like structures that grow in the lake and appeal to photographers from around the world. Calcium-rich water bubbling up from underwater springs combines with the lakes carbonate-rich waters in a chemical reaction to create the lime-based structures. Towers as high as 30 feet can be built under water through this process in a time span that may involve centuries.
The reason these towers are visible today is due to the unquenchable thirst of millions of people in Los Angeles. This thirst came close to destroying Mono Lake, as it did the Owens River and Owens Valley south of Mono Lake. Starting in 1941 the politically formidable Los Angeles Water and Power Company tapped into the streams flowing into Mono Lake and sent the water on a one-way, 330 mile journey south, reducing water in the lake from 4.3 million acre feet in 1941 to 2.1 million acre feet in 1982.
The United States Navy also posed a threat to Mono Lake by carrying out a series of under water explosion tests during the Cold War. The plaque at the site described these explosions as top-secret seismic tests. Whether the navy was searching for a way to predict earthquakes and tsunamis or cause them is the question. Fortunately, public pressure and concerns for public safety led to the navy abandoning its activities at Mono Lake in the late 50s/early 60s.
It was the growing environmental movement of the 70s and the Mono Lake Organization that eventually forced the Los Angeles Power and Water Company to reduce the amount of water it was exporting from Mono Lake’s tributaries. Today the lake is on the way to recovering its pre 1941 water levels (assuming it isn’t wiped out by global warming and drought). Mono Lake is found just north of Lee Vining off of Highway 395. Following Highway 120 west out of Lee Vining will take travelers into Yosemite National Park.

The Sierra Nevada Mountains provide a scenic backdrop in the west for Mono Lake. Highway 395 runs along the base of the foothills. Tufa can be seen emerging from the lake.

Following Highway 120 east off of Highway 395 will bring visitors to Mono Lake’s South Tufa Trail where the photos in this blog were taken. (Photo by Peggy Mekemson.)

Prior to Los Angeles tapping into the streams that provide water to Mono Lake, this tufa tower would have been underwater. Now it sits on dry land.

Reflections add extra character to this often photographed tufa island in Mono Lake— as they do in the next two photos. (Photo by Peggy Mekemson.)
NEXT BLOG: Having finished our desert series, Peggy and I return to Oregon and visit Oregon Caves National Monument.

Highway 395 is one of America’s most scenic drives. This view looking up at Mt. Whitney, center top, is one of the reasons why.
Highway 395, with its panoramic views of the eastern Sierra Nevada Mountains, is one of the most scenic highways in the United States. I will admit to a degree of prejudice, however. John Muir called the High Sierras the Range of Light. I think of them as ‘home.’ I have backpacked up and down the range numerous times. The mountains call to me in a way that no city or town does.

Driving up California’s Highway 395 provides an ever-changing perspective of the eastern Sierra Nevada Mountains.

Another view of the Sierra Nevada Mountains along highway 395. This seems to fit Muir’s Range of Light description. (Photo by Peggy Mekemson.)
I celebrated my 60th birthday by backpacking over 300 miles down the spine of the Sierras, I started at Squaw Valley, which is north-west of Lake Tahoe, and ended by climbing up Mt. Whitney. It was my sixth trip up Whitney. I figured it would be a fitting way to kick off my sixth decade.

Wrapping up five weeks of backpacking, my final climb looms in the distance. The curved mountain just to the right of my head is Whitney. I will be sitting on top the next day. The Sierras are fault block mountains, climbing gradually on their western slope and dropping off rapidly in the east. (Photo by Jay Dallen.)

And here I am on top, complete with a large grin. The Owens Valley and Highway 395 lie some 10,000 feet below. (Photo by Jay Dallen.)

Looking north from Mt. Whitney up the crest of the Sierra Nevada Mountains where I had just backpacked following the Pacific Crest and John Muir Trails.
The mountain’s claim to fame is being the highest mountain in the contiguous United States. It stands at 14,505 feet (4,421 meters). My friends in Alaska are quick to point out that Mt. McKinley/Denali is 20,322 feet. Mt. Shasta, where I began this particular series, is 14, 180 feet. And finally, for comparison, Mt. Everest, the world’s highest mountain, tops out at 29,029 feet (8,848 meters).
Once the snow has melted, climbing Whitney does not require any technical climbing skills. A good trail leads to the top. According to the plaque on top, it is the highest trail in the United States. It was started in 1928 and completed in 1930. The plaque used to (and still may) claim that the mountain is 14, 496.811 feet high, which would seem pretty darn accurate, especially given the .811 feet. Apparently modern measuring techniques have added a few feet. Not that it matters, unless you happen to be the person climbing those last nine feet.
Getting to the top requires stamina, lots of it. The eastern route up the mountain starts at Whitney Portal and climbs 6000 feet. That’s a bunch of up, and the higher you climb, the thinner the air becomes. Most people slow way down near the top as their bodies fight to get enough oxygen.
I’ve always started from the west since I am either ending or in the middle of a backpack trip. There are two advantages. Most important, I’ve already spent several days hiking at higher elevations. My body has both toughened up and adjusted to thinner air. Second, by starting at Guitar Lake, the climb is only 4,000 feet. Still that’s 4000 feet up and 6,000 feet down on a 15-mile day carrying a 40-pound pack— hardly a walk in the park. (Grin)
The reason for climbing the mountain, beyond being able to say you have, is the spectacular scenery. I wouldn’t recommend the trip for anyone with acrophobia (fear of heights), however, given that all of the views involve looking down several thousand feet.

My nephew, Jay Dallen, stands on the edge of a thousand foot precipice and looks down. He obviously does not suffer from acrophobia. Different people joined me on each of my five-week segments. Jay was 16 at the time.
The Alabama Hills, featured in the photo below, are located just outside of Lone Pine at the base of Mt. Whitney. Over 300 movies, mainly Westerns, have been filmed in the area. Almost every major Hollywood cowboy from the 1920s up to the present have made movies there. (Photo by Peggy Mekemson.)

We found this rather handsome fellow on our way up to Wildrose in Death Valley. Check out the shadow! (Photo by Peggy Mekemson.)
I crossed over the Panamint Range once on a bicycle. It wasn’t fun. Or let me put it this way, the nine-mile climb up out of Panamint Valley wasn’t fun. It was at the beginning of my 10,000-mile solo trip around the US. I only had seven days of cycling behind me so I was still getting in shape (massive understatement). Adding to the challenge, I was carrying over 50 pounds of gear, everything I needed to survive six months on the open road.
Standing out of the saddle in my lowest gear, and exerting every bit of muscle power I could, I averaged two miles an hour. And yes, it would have been much easier to get off my bike and push. But I am a stubborn when it comes to things physical. The ride down, on the other hand, was lovely and about 20 times as fast.
Our Toyota Tacoma thought nothing of the climb out of Death Valley to the Emigrant Canyon Road and on to Wildrose Canyon. In fact the pickup loves a challenge and likes to be on the road as much as Peggy and I do. Or maybe I am anthropomorphizing a bit too much here. (And don’t you just love that word, all 18 letters of it.)
We were lollygagging along on the Wildrose road and stopping often to photograph flowers when we passed the rattlesnake. Peggy was driving. “Stop, back up,” I urged. Laughing, Peggy complied. She’s used to my fascination with rattlesnakes. I’ve had dozens of encounters over the years. One of my favorite tricks is to get down on my belly in front of them to take photos as they crawl toward me. Unfortunately, my headshots are usually blurry. Could it be that I am backing up too fast?

Having determined that we weren’t edible, the large snake went on his way. Isn’t the head magnificent? It shouts pit viper.(Photo by Peggy Mekemson.)
This guy was a beauty, a Panamint rattler (Crotalus stephensi), and I would guess almost record size. He was on the driver’s side of the truck so I handed Peggy her camera and she snapped three shots. And then, before I could get out to the truck for some close-ups, she stepped on the gas and we were out of there. Can you imagine that? I whined for an hour.
The flowers soon assuaged my disappointment, however. At our elevation of around 5,000-7,000 feet, they were everywhere. While we were too late to catch flowers blooming in the valley, our trips up to Dante’s View and Wildrose more than made up for it.

I was taken by this old desert road that cut off the main road and was covered with flowers as far as the eye could see.

These prickly poppies were attractive. Petals were tissue paper thin. The red beetle was quite busy.

I don’t know what this striking yellow beauty was. Maybe one of my readers can identify it. (Finally found it in one of my field guides. It’s called Desert Plume and is a member of the mustard family.)

This lupine, however, is an old friend. It is common throughout the west. Peggy is even growing some. What was amazing about this plant was its size. I would say around four feet tall.
Beyond the rattlesnake and the flowers, the highlight of the tour was the ten charcoal kilns built in by the Modoc Consolidated Mining Company in 1877 to prepare charcoal to be used in smelters at its lead-silver mine about 25 miles away. Local pinion pines and junipers were cut down and hauled to the kilns. It took approximately four cords of wood to fill one kiln. After 6-8 days for burning and another 5 days for cooling the charcoal was then transported by an army of jackasses.

The kilns, which were used for about three years, have sat quietly for over a century. Navajo Indian stonemasons from Arizona restored the kilns in 1971. (Photo by Peggy Mekemson.)
An interesting aside is that George Hearst was the principal investor in the mining company. His son, William Randolph Hearst, would go on to found the Hearst media empire. And it was his great grand-daughter, Patty Hearst, who was kidnapped by the Symbionese Liberation Army in the 70s. Where this is going is that I met Patty and her abductors in the Sierra Nevada Mountains. I was up with some friends scouting out streams for trout fishing when a van roared around us and got stuck in a snow bank, which we found rather amusing. A group of folks came tumbled out of the van including a young woman who came over to talk with us while her companions tried to dig out of the snow.
“Do you have any guns in your car?” she asked. “My friends have been teaching me how to shoot automatic weapons in the Bay Area and we are up here for practice today.” That’s when the alarm bells started going off for me. We were talking to Patty Hearst and her ‘friends’ were SLA members. When Patty wandered off to check on the van’s progress, I whispered my concerns to my friends and suggested we help get the van on its way, which is what we did.
But so much for the detour (grin). I was either going to tell you stories about rattlesnakes today or the Patty Hearst. Patty won. Back to the kilns.

A final view from Wildrose. What appears to be puffy white clouds on the horizons are the snow-covered Sierra Nevada Mountains.
NEXT BLOG: What’s a desert without a ghost town, or two. We head off to the old mining town of Rhyolite sitting on the edge of Death Valley.
Zabriskie Point is one of the most photographed spots in Death Valley. Tour busses stop here and disgorge thousands of passengers annually. Everyone comes armed with a camera, or at least a cell phone camera. Twenty shots or so later they are on their way, scurrying back to the bus and Death Valley’s next must-see sight. We are more leisurely in our approach, but we also take a more photos. Erosion is king here, wearing away rocks that were deposited in a lakebed some five million years ago– back before tectonic forces created Death Valley and back before the region became a desert.

As in other parts of Death Valley, the rocks of Zabriskie Point are multi-hued. (Photo by Peggy Mekemson.)

Peggy and I were at Zabriskie Point in the late afternoon. The rocks above Manly Beacon seemed to take on an inner glow.
A three-mile trail leads down to the Valley floor from Zabriskie Point and passes through Golden Canyon on the way. For fans of Star Wars IV, segments of the movie were filmed in Golden Canyon. The diminutive, eye glowing Jawas captured R2-D2 and C-3PO there. So you can think of Death Valley as Tatooine, the home planet of Luke Skywalker. (Tunisia was also used for scenes on Tatooine.)

Golden Canyon looking out toward Death Valley. This photo and the one below were taken from an earlier trip. R2-D2 and C-3PO were captured in the canyon by the Jawas.
Here’s some Star Wars trivia I picked up when doing research for this blog that you can use to wow your friends: sounds made by dogs, bears, lions, tigers and walruses were combined to create Chewbacca’s voice.
The Twenty Mule Team Canyon that I blogged about in my last post starts a mile or so above Zabriskie Point. A few miles farther, a road jogs off to the right that leads to Dante’s View, which towers some 5000 feet above the valley floor. The last part of the road is steep and narrow but the view is worth it.

I took this final photo from Dante’s View to capture the very impressive alluvial fan spreading out on the Death Valley floor far below. Debris coming down off the mountain had built this fan up over thousands of year.
NEXT BLOG: Traveling into the Panamint Range of Death Valley: wild flowers, huge charcoal kilns, and one very large, irritated rattlesnake.

Prepare to be dazzled with a kaleidoscope of color on a drive through Twenty Mule Team Canyon in Death Valley. Various minerals are responsible for the colors.
Death Valley is a land of superlatives. Think hottest, lowest, and driest place in North America. It holds the world record for heat at 134 ˚ F (57˚ C). Ground temperatures have actually been measured at 201˚ F. As for rainfall, there are years without any and the annual average is 2.36 inches (60 mm). Finally, a trip into Badwater Basin, easily reachable by car, will drop you down to 282 feet below sea level.
Given these extremes, a person might wish to travel to Death Valley for the sole purpose of saying he or she has been there. (Or conversely avoid Death Valley passionately.) But from my perspective, the reason for visiting Death Valley is its exotic beauty. Over the past three weeks, I’ve taken you to the Valley of Fire and Red Rock Canyon. Not bad on scenery, eh? Consider it a warm up.
I’ve been to Death Valley numerous times and have blogged about it in the past. On our recent trip, we climbed out of the valley and explored other parts of the National Park including Twenty Mule Team Canyon, Dante’s View, Zabriskie Point and the unusual Charcoal Kilns high up in the Panamint Mountains.
Today, we will begin our journey with a drive through the colorful badlands of Twenty Mule Team Canyon. Imagine for the moment, taking 18 mules and two horses, hitching them to a huge wagon, and hauling 10 tons of borax over desert terrain for 160 miles. That is how borax was hauled out of Death Valley between 1883-1889 and it has become part of the local lore and legend. Francis Smith, the founder of Pacific Borax was also a first class promoter and sent his mule teams out to major cities across the US to push his soap products. At one point, they paraded down Broadway in New York City.

This early, unattributed photo in the public domain, provides a view of the 20 mule team with its Death Valley backdrop. The driver had a very long bullwhip to encourage his mules along the way.

The mules were eventually replaced by a steam tractor. “Old Dinah” is featured at Furnace Creek. Dinah, in turn, was replaced by a railroad.
Twenty Mule Team Canyon was never part of the route the mules followed. So why the name? It could have been to honor the teams but I suspect it was the bright idea of a tour agent. Whatever, no harm was done. Twenty Mule Team Canyon provides a kaleidoscope of color, a laboratory of erosion, and a fun drive.

The 2.8 mile road through Twenty Mule Team Canyon is a fun drive but it isn’t made for large RVs or fifth wheels. (Photo by Peggy Mekemson.)

A number of trails wander off into the rocks, inviting visitors to stay for a while and explore. (Photo by Peggy Mekemson.)
NEXT BLOG: We check out what is probably the most photographed area of Death Valley, Zabriskie Point, and climb 5000 feet above the valley to Dante’s View floor for a bird’s eye perspective.

Depending on traffic conditions, Red Rock Canyon National Conservation Area is 30-45 minutes outside of Las Vegas. It is hard to imagine two more diverse worlds.
Las Vegas shouldn’t exist.
Why would any sane person build a city in middle of a desert where summer temperatures regularly climb over 110 degrees F and annual rainfall hangs around 4 inches? Sure, it’s a great place for jackrabbits and rattlesnakes and scorpions and cacti and desert tortoises. Maybe even lonely miners, ladies of the evening, jet jockeys, crotchety cowmen, and aliens belong there.
But putting 1.8 million people into Las Vegas and the surrounding Clark County– what were they thinking? Everything has to be imported… and I mean everything including the ever-precious water for golf courses and tourists with bucks to toss. Cut off either one and Las Vegas is SOL. The city returns to the jackrabbits and LA sucks up any extra water from the Colorado River.
MONEY, of course, is the answer for the city’s existence– obscene amounts of it, like bundles and bundles and bundles. Mafia hit men joined together with Mormon bankers following World War II to build the Flamingo Casino and start milking the proverbial cash cow. This kicked off a spree of building pleasure palaces that continues even today, with each one being bigger and glitzier than the one before. The names and faces have changed, but the basic underlying purpose remains the same: separate tourists from their hard-earned cash, as quickly as possible.

Down around Fremont Street, a touch of Old Vegas where mobsters ruled has been preserved. If you go down there, and you should, be sure to visit the mobster museum. The cowboy above would have been the epitome of neon lighting in its day.

Most of the older casinos in Las Vegas have now been replaced with fantasy creations that out-Disney Disney.
Now I confess to liking a little glitter from time to time. A stroll down the Strip drops me into Venice, New York City, Paris or even a pyramid. While pale in comparison to the real thing, the moguls of Las Vegas have spent billions creating these make-believe worlds. And the price of admission is right: free. At least it is if you can avoid the multiple temptations. I can’t. I am sure there is a quarter video poker machine out there that will make me rich beyond my wildest dreams, or at least pay for dinner. Or, failing all of that, cover the tourist tax. (Remember here, however, that I also believe in UFOs.)
There comes that inevitable moment, however, when I have to escape the glitter, noise, and crowds for the wilderness. I have to return to my roots, to commune with nature. Luckily, it’s easy from Las Vegas. Last week I took you out to the Valley of Fire, a short hour drive away. Today we are going to visit Red Rock Canyon National Conservation Area, which is even closer, 30–45 minutes.

Truth be told, if I have to choose between urban fantasies and natural wonders, I’ll go for the natural wonders. We found this desert tortoise outside the Red Rock Canyon Visitor Center but you might see them anywhere in the park, as the sign below attests.
This gem sits on the edge of Las Vegas. An easy morning trip will get you there, around the park and back. The park features a one way, 13-mile drive with numerous turnouts. There are several hiking trails that crisscross the area. Many people also enjoy biking the route. I highly recommend starting your trip at the excellent visitor’s center.
Here are some views along the way.

Be sure to stop off at the Visitor’s Center for an overview of Red Rock Canyon. In addition to having excellent information on the park, it includes lots of fun things like this kid-sized snail sculpture.

You can also preview your route from the Visitor’s Center. The road snakes around the colorful hill in the foreground. (Photo by Peggy Mekemson.)

A close up of the same hill taken from the road. One of Red Rock Canyon’s many hiking trails is seen at the base of hill.

As in the Valley of Fire, the various rock formations in Red Rock Canyon are carved out of ancient sand dunes that have been turned to rock. Peggy captures one of the formations here.

Pull offs from the road provide a number of opportunities to stop and admire the scenery. I took this shot from the Sand Stone Quarry pull off.

We found these Native American pictoglyphs near Willow Springs. Petroglyphs are made by pecking the rock surface with a rock. Pictoglyphs are made with natural paint derived from minerals. flowers, etc. The pigment for these handprints came from hematite, iron oxide.

I thought these twin cactus flowers would provide a fitting conclusion for my blog on Red Rock Canyon National Conservation Area.
NEXT BLOG: Hello Death Valley!