Station P085

Science Spotlight


Researcher: Bill Hammond
University of Nevada, Reno

I like my job because I get to dream up wild explanations that help us interpret and understand the data in terms of Earth processes!


P085 is located near Battle Mountain, Nevada.


Name: SLAVENCYN
State: NV
Country: United States
Elevation: 1661.8 m
Lat/Long:  40.4955 / -116.7362

Basin and Range Deformation

The many mountains of the Basin and Range in Nevada were created in response to slow, region-wide tectonic extension that is breaking the Earth's crust along fault lines.

Here, the Earth's surface is part of an 800-km-wide zone of slow deformation of the North American plate. The terrain is responding to the motion of the Pacific plate to the northwest and the weight of the high elevation intermountain western U.S. Cumulative displacement along these faults over long periods of time built, and is still building, topographic relief, i.e. the valleys and ranges. Earthquakes associated with infrequent slip on these faults generate the seismicity felt by people who live in the Great Basin and Sierra Nevada.

In my research I use GPS to measure the processes behind growth of mountains and generation of earthquakes in the Basin and Range and Sierra Nevada. GPS provides precise measurements that let us understand the style and distribution of Earth surface deformation that is a direct consequence of continent-scale tectonic processes.

Data from station P085 shows that central Nevada moves 2.9 mm/yr (yes, *millimeters* per year!) with respect to points east of Salt Lake City, Utah. We can also see that points in California move a little faster than station P085, showing that the crust is stretching west of P085. For example, PBO station P349 moves west 6.6 mm/yr, so there is ~3.7 mm/yr of east-west stretching between those two points.

In tectonic geodesy we are interested in the slope of the GPS position time series that indicates the steady rate of motion of the station. The data show a position for each day (blue dots). Slow and steady motion is the effect of the drift of Earth's crust under central Nevada with respect to the rest of the North American plate.

Measurements of this sort have been made at many stations in the Great Basin and rest of the world. Figure 3 shows the measurements from hundreds of stations in Nevada. These show a slow steady changes of rates across the region, a smoothly varying deformation field illustrating the stately flow the Earth's crust.

Figure 1. Basin and range topography from the air. (Photo: Marli Miller, University of Oregon, via Earth Science World Image Bank)


Figure 3. GPS station P349 is 470 km west of P085 and moving west faster than P085 by nearly 4 mm per year.


Figure 5. Position changes for P085 in a North America fixed reference frame. (For help interpreting the graphs, see the GPS Data page.)

 

Figure 2. A basin and range valley leading up to a mountain range. (Photo: Bill Hammond)


Figure 4. A cross section of basin and range geology, also know as horst and graben.


Figure 6. The extent of the Basin and Range province. (Credit: National Parks Service)

Spotlight Questions

  • Is this site moving east or west with respect to stable North America?
  • What parts of Nevada stretch quickly? What parts stretch slowly?
  • How does stretching the Earth's crust build mountains?

Copyright © 2012 - 2017 GPS Reflections Research Group. All Rights Reserved. | Funding.
Please send comments and corrections on this website to gps.reflections@gmail.com
Supported Browsers: For best performance, use the latest version of one of the following browsers: