Showing posts with label desert. Show all posts
Showing posts with label desert. Show all posts

Monday, April 27, 2009

Desert Destination: Black Rock Lava Flow

Every Monday we visit a Desert Destination.
Out in the middle of the three-hour long drive between Ely and Tonopah, with no public bathrooms, no telephones, no gas, and no soda machines, part of US Highway 6 passes through the Lunar Crater Volcanic Field. A BLM sign alerts drivers who are still awake about the nearby Black Rock Lava Flow. You can see it from the highway, but it's much more interesting to take the one-mile detour (the sign says two miles, but it's wrong), and get out and stretch your legs a bit.

A sign gives some information about the lava flow with the unimaginative name. The lava flow is made of basalt. Hot lava swelled up inside the nearby cinder cone and broke through the walls, flowing towards the west. As the lava cooled, it solidified. The Black Rock Lava Flow is the youngest of the lava flows in the lunar volcanic field, and covers about 1,900 acres.

Behind the lava flow are a couple of the many cinder cones in the area. The entire Lunar Crater area in central Nevada encompasses about 100 square miles and includes more than 20 extinct volcanoes and 35 lava flows. You can read a bit more about the geology of the area on this USGS page.

I was a little surprised when I walked up to the lava flow to see that not all of it was solid lava, like I've seen at other lava flows. The south edge of the lava flow has many scattered pieces of basalt.

Among the basalt are bushes and dirt--and probably quite a few wildflowers right about now.

I visited in March, when the temperatures were wonderful for exploring. In the middle of the summer, this area can be scorching, with the black basalt absorbing the hot desert sun. In the winter, it can be covered in snow.

The basalt hosts an interesting array of lichens. Here's an interesting post about lichens in the Salt Lake area. They certainly lend more color to what might be described as a rather stark view.

I should mention that the Black Rock Lava Flow is many hours away from the Black Rock Desert, where the (in)famous Burning Man Festival is held every year. 

Embedded in some of the basalt are rocks and crystals that the magma picked up deep within the earth on its way to the surface.

Lizards love to hang out in the lava field.

The road continues on around the lava field, where it becomes more continuous. I didn't have time to see the entire lava field, so when I got home I took a look at Google Earth and found this image of the lava flow (I added the labels):

As you can see, the lava flow really stands out from the surrounding scenery. Not too far away is Lunar Crater, a maar about 4,000 feet across and 400 feet deep. I hope to get there soon!

Monday, April 13, 2009

Desert Destination: Death Valley

Welcome to Death Valley National Park, at over 3 million acres, it's the largest national park in the lower 48 states. It's a place full of colorful geology, unexplained phenomenon, extreme variations, and wonderful surprises.

On today's trip, I'm going to take you from the southeast end of the park, near Shoshone, along the road that traverses the eastern side of the park up to Scotty's Castle.

Spring is a great time to visit Death Valley. Not only are the temperatures reasonable, but desert plants brighten the landscape. Some of the best places to see flowers are right next to the roads. Just park and wander around, and the diversity of life becomes apparent.

One of my favorite plants, the creosote bush (Larrea tridentata) was in bloom. 

The bright yellow flowers flashed as the branches waved in the wind. 

Spring is a popular time to visit Death Valley, and in fact there were thousands of people staying at Furnace Creek, the park headquarters area. But because Death Valley is so huge, people are spread out in the rest of the park, and it often felt like I had it all to myself.

It was easy to pull off the highway and snap photos of whatever caught my attention, like some more wildflowers and the beginning of a salt flat.

The salt makes it hard for vegetation to live, but nevertheless, some plants and animals have adapted to it. One of the reasons there is so much salt in the bottom of Death Valley is that it used to have a huge lake in it, Lake Manly. When the water evaporated, the salt was left behind. The lake fluctuated at different levels, so there were many opportunities for salt to be deposited.

As I headed north, I noticed some people walking out on a big salt flat. I rounded a curve and saw a parking area. This wasn't just any salt flat, it was...

...Badwater! The lowest spot in North America, at 282 feet below sea level. A boardwalk stretched out from the parking lot onto the salt flat. 

I was there late in the day, but I could just imagine the heat of a July sun at noon. It would probably be over 120 degrees Fahrenheit, about hot enough to start drying a person into jerky.

These holes intrigued me. I'm not sure what caused them, but it makes me wonder if there are parts of Badwater that might suddenly sink and swallow me up.

Off the beaten path, the salt deposits rise up and provide interesting relief.

At Devil's Golf Course, the salt formations are even higher. They look delicate, but most are very hard and crunchy. Footing is difficult, and a fall would hurt.

Since it was late in the day, for a short while I was the only one out there, and it felt both neat and creepy at the same time.

I decided to take a detour off the highway to go on Artist Drive. The mountains are particularly colorful in this area. With the sun mostly behind Telescope Peak and the other mountains on the other side of the valley, I didn't have the full effect of the artist's palette, but it was still spectacular. The road is one way because of some tight turns and constricted canyons. Maybe next time I can do it on bicycle.

The next day I got a really early start and continued further north to Salt Creek. This is a little creek on the valley bottom. Despite the high salt, high temperatures, and scarce vegetation, this creek manages to be home to tiny pupfish, along with aquatic insects, birds, and more. 

A sand dune with pickleweed is right near the trail. The pickleweed is succulent, with squishy flesh that stores water.

To protect the creek, the trail is on a boardwalk which goes next to and sometimes over the creek.

Further north I found more good places to stop and enjoy the wildflowers.

It was a very windy day, so I decided to skip the sand dunes near Stovepipe Wells. In the distance of this photo you can see the sand blowing off the dunes. If you want to experience a sand storm, one way to get a similar feeling is go to sand dunes on a windy day. I'm not sure why you would want to experience a sand storm, but just in case...

There is just so much to see in Death Valley that at times it becomes visually overwhelming. One thing I like to focus on are the alluvial fans, the land flowing out of the canyons in a fan-like pattern. Water eroded the rock away further upstream, redepositing it. As I look at the alluvial fan, my eye always moves up to the mouth of the canyon and I wonder what is up there. Death Valley must have hundreds of alluvial fans, so it makes my imagination go wild.

Another stop to admire some beautiful phacelia. Flowers bloom at the lower elevations from about February to the end of March, and then they start blooming at higher elevations. Telescope Peak is over 11,000 feet high, so there are even flowers blooming in the middle of summer in Death Valley.

A couple more alluvial fans coming down from mountains on the other side of the valley, with creosote bushes in the foreground.

Towards the north end of Death Valley, the main road curves to the east and goes to Scotty's Castle
The area is an oasis, and it's fun to wander the grounds and feel a little more humidity. A hummingbird was hanging out near the small waterfall between these palm trees.

Continuing up Grapevine Canyon, the road eventually leaves the park. I like the back of the park entrance sign, which said "Thanks for Experiencing Your National Park. Please Visit Again." 

I think I will. Thanks, Death Valley.

Monday, April 6, 2009

Desert Destination: Goldstone Deep Space Communications Complex

Every Monday we visit a desert destination.
A few weeks ago I had the opportunity to visit a desert location that makes one realize how small our planet Earth is. That place was the Goldstone Deep Space Communications Complex, which has an array of antennas that communicate with spacecraft that might be billions of miles away. 

Yikes. I can't even fathom that distance. And to imagine we have communications that far away? Why, we don't even have cell phone coverage where I live, how can we possibly communicate with tiny little spacecraft we can't even see anymore?

Goldstone is located on the Fort Irwin Military Base about 35 miles north of Barstow, California.
When driving towards Fort Irwin, I noticed some signs that I don't usually see. 

The tank next to the Welcome sign provides an interesting message, especially with the gun pointed right at the cars driving on the highway!

After going through the security booth (which took awhile--I felt like I must be a decent human when they finally finished checking my documents and didn't find me appearing as wanted on any of the government databases), I headed down the road marked as Ammo Route. I'm not quite sure what that was about...and I wasn't sure I wanted to ask!

The desert skies darkened and opened, allowing a deluge of water to fall upon the desert. I managed to snap a photo of the entrance sign to Goldstone, but my windshield was splattered with rain drops. 

The road to the main Goldstone complex is fascinating. Tucked away in the creosote bushes are huge antennas, pointed in different directions up in the sky. They are placed in basins so that the surrounding mountains block stray signals from other sources.

The different arrays are given different names, some after planets, like the Venus station. 

At the main Goldstone complex, our group went into a classroom for an excellent presentation from the outreach coordinator, Karla Warner. Our group was the maximum size of 50, but groups as small as a single family can also go on the tour. Generally two tours a day, four days a week are given. Reservations are required by calling Karla at 760-225-8688 or emailing her at kwarner@gdscc.nasa.gov. About 4,000-5,000 people a year tour the Goldstone complex.

After the presentation, we had time to peruse the exhibits that covered a range of space-related themes.

Then it was time to go 12 miles further into the complex to the Mars Station, home of the largest antenna, 70-meter Mars. You can see how big it is compared to the tiny cars in the bottom right of the photo. 

Side note: Do you see all the bright blue sky? The storm dumped for about 20 minutes and then was over.

The antenna is so large because the signals coming from space can be extremely weak--as weak as a billionth of a billionth of a watt--20 billion times less than the power required for a digital wristwatch.

The shape of the antenna is extremely important to hear the whisper of the signal coming from tiny spacecraft so far away. To help figure out what the signal is, the extremely sensitive receivers use amplifiers that are cooled to within a few degrees above absolute zero (-273 degrees C; -460 degrees F) to reduce the background noise generated by the electronic equipment.

The antennas also send signals to the spacecraft, telling them to turn on computers, take photos, activate instruments, and make course corrections. 

Here are just a couple rows of equipment that are used to record the data received. There are many more rows in this section of the building. And another part of the building is used to house the data to be sent. 

Goldstone is in California, a state known for its earthquakes. So above all this sensitive equipment are round beams that the equipment cases are connected to. A strong earthquake might make the floor rattle and roll, but the computers and recorders will be safe.

California is not always in the optimum position to talk or listen to spacecraft because of the earth's rotation, so there are two other deep space facilities: near Canberra, Australia and near Madrid, Spain.
Here's a glimpse into the control room at Goldstone. Different computers control different antennas. For routine communications, 34-meter beam-waveguide antennas are the most common. Other types of antennas include high efficiency, azimuth-elevation, and hour-angle declination. (I really don't know what those mean, but I'm trying to sound intelligent. I remembered to take a little brochure with me from the tour so I could get my facts straight, because there's no way I could have remembered all this.)

And if you'd like to make sure I haven't told any lies--or you just want to learn more, you can visit the Deep Space Network website.

On the drive back out of Goldstone and Fort Irwin, I passed several desert tortoise crossing signs, but unfortunately didn't see any desert tortoises.

However, I did see a sea monster making its way across the lake dry bed. I would have liked to have stayed longer to make its acquaintance, but I was a little afraid because I was on the Ammo Route, and I still didn't know what that was.

I saw a sign before a bridge that declared the weight limit was 64 tons. I didn't think that was for the sea monster.

Sure enough, there were more tank crossing signs. The brake marks on the pavement make me wonder if someone didn't take the sign seriously enough.

And finally we reach the end.
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