Showing posts with label Spring Mountains. Show all posts
Showing posts with label Spring Mountains. Show all posts

Friday, March 25, 2016

A Sight That Overwhelms: Dante's View and a Sense of Scale

It's one of the most astonishing viewpoints in all of North America. The Black Mountains form the eastern edge of Death Valley, and they are one of the most rugged mountain fronts in existence. In places the mountains are so steep that one cannot see the slopes at the base from the summit. Looking up from the lowest point in North America, Badwater, one can barely contemplate walking or driving to the summit across the barren cliffs.
And yet a road does just that. Taking advantage of the asymmetrical nature of the range, a paved road winds up the eastern flanks, and only the last few hundred yards of the drive are a vertiginous nightmare. And then there is a view like no other.
Death Valley is the largest national park in the lower forty-eight states, and Dante's View takes in much of the park, offering on clear days a view that extends across more than a hundred miles of desert ranges and salt flats. The view is so unlike any other place on the planet that George Lucas used it as setting for his alien planet in some movie about wars across the stars ("Mos Eisley spaceport. You will never find a more wretched hive of scum and villainy.").
Even though the summits reach nearly 6,000 feet above sea level, the slopes are barren and dry. The range lies in the rain shadow of the Sierra Nevada and two other high mountain ranges, including the Panamints that rise to 11,000 feet on the other side of Death Valley. In any other mountain range, 6,000 feet would support a thick forest. Here in the Black Mountains, only sage and seasonal wildflowers can grow.

The lack of vegetation is a boon to the geologist, of course. The exposures of bedrock are unparalleled, revealing a great deal about the geologic history of this part of the world. And it is a strange story. Much of the mountain range is composed of the Black Mountain Metamorphic Complex, a selection of gneiss and schist sequences that reveal evidence of a titanic series of plate collisions 1.7 billion years ago. At that time, North America was hit by a series of terranes, island systems maybe the size of New Zealand or California. The collisons produced a mountain range hundreds of miles long that would recall the coastal ranges of southern Alaska, minus the rainforests (terrestrial life didn't arise for at least another 1.2 billion years). These rocks are related to those found in the depths of the Grand Canyon and farther south in Arizona and New Mexico.

In the ensuing years, the vast range would be eroded to a nearly flat plain, and the surface would eventually subside below sea level. Tens of thousands of feet of Paleozoic sediments covered the rocks so they lay hidden deep in the continental crust. In the last few tens of millions of years, the regional crust was stretched and extended, and the overlying rocks slid away, causing the Black Mountains to "pop up" in the geologically short stretch of two or three million years. The exposure of the deep crust was accompanied by violent caldera eruptions, and parts of the mountain range are covered by colorful ash deposits (the rocks along Artists Drive Loop are particularly memorable).
Some places are so overwhelming that one can lose a sense of scale while staring into the abyss. Take a look at the picture below: we are looking at the vast salt pan of the Badwater Basin, the lowest place in North America at minus 282 feet. The salt flats cover 110 square miles. How big an area is this?
To find out, take a look at the thin channel of salt marked with the arrow in the picture above. We'll zoom in a bit, and find that we are looking at a spot next to the Badwater parking lot, which is just out of sight at the bottom of the picture. One can make out the Badwater Road on the left side of the photo. What are those dots on the salt channel? Let's zoom in a bit more (120x by now).
They're tourists! Badwater is a main destination for visitors to Death Valley. The stop lies 5,700 feet beneath Dante's View, and only two miles west. These mountains are about as steep as any can be.
The view from Dante's View on this afternoon in February was unique for me. Flash floods in October had destroyed some roads in the park, and I found it necessary to alter our usual itinerary. We usually see the viewpoint in the early morning. Until this day I had never seen the sun set over desert like this. It was an astounding sight. Even overwhelming...

Saturday, May 10, 2014

Where are the Ten Most Incredible Places You've Ever Stood? My Number 3: Standing over Dante's Inferno in the Broken Lands

The Panamint Mountains and Telescope Peak, the highest part of Death Valley National Park, as seen from Dante's View..
Death Valley is the hottest place on planet Earth.  Furnace Creek recorded a temperature of 134 °F (57 °C) in 1913. With the dethroning of the improperly recorded temperature in Libya from 1922, this is the hottest officially recorded temperature in world history. Badwater, a dozen miles south of Furnace Creek at the deepest point in the valley, is often a few degrees hotter. The hottest overnight temperature ever recorded, 107 °F (42 °C), was measured here on July 12, 2012. That day, the average temperature was 117.5 °F (47.5 °C), the world's hottest 24-hours on record.

Hot temperatures are an interesting feature of Death Valley National Park, but the park is much more significant for other reasons. It contains a wider range and variety of rocks than any other park that I know of. I have been chronicling our February journey to Death Valley over the last few months in a series called "Out of the Valley of Death", and today's post is a confluence of the two series that I've been working on. Dante's View was our next stop after exploring the interior of an upside-down mountain at Titus Canyon, and it makes number three on my list of the Ten Most Incredible Places I've Ever Stood.

The Black Mountains of Death Valley are one of the most rugged mountain ranges in existence. They rise 6,000 feet almost straight up from the lowest part of the Death Valley graben and are practically devoid of trails or roads. The thought of climbing the mountain front near Badwater is as daunting a challenge as I can imagine. The Proterozoic metamorphic rocks are highly deformed and internally sheared by intense faulting, making for a highly unstable climbing surface. But there is a way to the top of the range. A paved highway winds up the other more gentle eastern side of the mountain range, reaching Dante's View at an elevation of 5,476 ft (1,669 m). The overlook is directly above Badwater, more than a mile below at -282 feet ( -86 m). It has one of the most incredible views to be found in any national park.
Frank DeCourten called the Basin and Range province where Death Valley is located the "Broken Land", and the description is apt. From Dante's View, thousands of square miles of land are visible as range after range marches off into the distance. In the last few million years crust in this region was stretched beyond the breaking point, and it broke into countless grabens (fault valleys) and horsts (fault-block mountain ranges).  River drainages that once reached the sea do so no longer, and water leaves the region only by evaporation. The region is sometimes called the "Great Basin" despite the multitude of mountain ranges. Death Valley is the lowest of the low, the ending point of numerous desert washes and the Amargosa "River" that sometimes in wet years has water.

At Dante's View, one's attention is most often drawn towards the salt pan of Death Valley, the lowest land in North America (in the picture above). It is quite a sight, and so alien-looking that it stood in as the location of Mos Eisely in the original Star Wars. Obi-Wan Kenobi and Luke Skywalker stood here, looking at the spaceport and mentioning that "You will never find a more wretched hive of scum and villainy". The salt that covers the valley floor to a depth of hundreds of feet was washed out of the marine sediments that make up many of the mountains in the region, and from the rain itself. Water flows into the salt pan and evaporates, leaving behind the salt and other minerals, including gypsum and calcite.
The view from Dante's encompasses, well, the entire compass. To the south (above) the Black Mountains continue for several miles, including two of the gigantic "turtleback faults". The rocks are some of the oldest in the western United States at 1.7 billion years. The dark metamorphic rocks gave the mountains their name. Although the slopes are not as hot and dry as the valley floor, it is still a tough environment for most plants. The mountains are as barren as any I've ever seen.
To the north (above), the Black Mountains include younger volcanic rocks dating from the middle and late Cenozoic era. They include the Artist Drive Formation, and the ancient lake and valley sediments of the Furnace Creek and Funeral formations. The Grapevine Mountains rise in the far distance. They are composed of thick sequences of marine sediments dating from the Paleozoic era. The farthest ranges are more than 60 miles away.
To the east (above), range after range culminates in the snow-covered Spring Mountains above Las Vegas (did you know you can ski near Las Vegas?). The highest peaks exceed 12,000 feet. Some of the water that accumulates on the slopes of the Spring Mountains travels underground through the intervening mountains to emerge as springs in Death Valley.
One of the most amazing things about the view from Dante's is how different it would have appeared 20,000 years ago during the last of the ice ages. Meltwater from the glaciers of the Sierra Nevada drained into the Great Basin, filling one valley after another until it spilled over into the Death Valley graben, forming a 600 foot deep lake more than 100 miles long.The lake left behind shorelines and terraces in what is currently the driest place in North America, and at least four species of native fish which still live in isolated springs around the park.

Water still accumulates in the Death Valley graben on occasion. Lakes were there in 2005 and 2010, but the same wet weather that filled the salt pan with water also wreaked havoc with the road to Dante's View and it was closed, so I have no pictures of the lake from above. This one from the valley floor will have to do.

Some of my choices for the "ten most incredible places" involved lava, or fossils, or significant historical and geological events. I chose Dante's View for sheer grandeur. From the high vantage point of Dante's, one gets a sense of being on top of the world, a world that is sometimes an inferno, and certainly broken up. There are few places on Earth like it.