Death Valley is approximately 200 km long and varies from 8-25 km in width, with 1-3 km deep sediments filling the steeply walled valley (Hussein et al, 2011).
Dante's View overlooks Death Valley from an elevation of 5474 feet (1669 m). If you can get up before dawn to get there, you will be rewarded by a gorgeous sunrise behind the peaks to the east and you'll see the light creep down into the valley. Some of my sunrise photos are at the end of this post.
Dante's View is on the Black Mountains which have been uplifted along the still active Black Mountains fault zone (Miller, 2005). Across the valley are the Panamint Mountains. From Telescope Peak (the highest point in Death Valley National Park) to Badwater Basin (the lowest point in North America), there is an elevation difference of 11,331 feet (3455 m).
|~11,000 feet (3000 m) of elevation change|
Death Valley is a classic example of Basin and Range topography: uplift of mountains along parallel normal faults leaves linear valleys between the mountain ranges (Hill and Troxel, 1966). It is also a great place to see alluvial fans. It's hard to get a sense of how big alluvial fans are unless you can see just how thick they are:
|Daylight has almost reached the tops of the alluvial fans. |
Yes, they really do go nearly halfway up the mountains!
|In the early morning light, shadows mark the canyons that feed the alluvial fans. |
The shadow of the Black Mountains still covers most of the alluvial fan and the valley floor.
|Many channels can be seen flowing down the fans|
|Panamint Mountains and the shadow of the Black Mountains in Death Valley.|
Hill, M., and Troxel, B., 1966, Tectonics of Death Valley region, California: Geological Society of
America, v. 77, p. 435–438.
Hussein, M., Serpa, L., Valasco, A., and Doser, D., 2011, Role of sedimentation in continental rifting
from comparing two narrow rift valleys the Salton Trough and Death Valley-California: Natural Science, v. 03, no. 11, p. 927–935.
Miller, M., 2005, Geological landscapes of the Death Valley region: Earth-Science Reviews, v. 73, no.
1-4, p. 17–30.