Skip to main content
U.S. flag

An official website of the United States government

Rebecca L. Kramer

I am a field instrumentation specialist working to support monitoring of volcanoes in the Cascade range.

I coordinate network topology, station design, and field operations for the Next Generation Rainier Lahar Detection System, working with partners including Pierce County and Mount Rainier National Park. I also provide network and field support for monitoring stations on Cascade volcanoes throughout Washington and Oregon. Additionally, I am a geodesy enthusiast and am often working to maintain and improve CVO's GNSS station infrastructure and data management.

 

Education and Certifications

  • B.S., Geophysical Engineering, Colorado School of Mines- 2009

  • M.S., Geophysics (Solid Earth), New Mexico Insitute of Mining and Technology - 2013

Science and Products

Combining InSAR and GPS to determine transient movement and thickness of a seasonally active low-gradient translational landslide

The combined application of continuous Global Positioning System data (high temporal resolution) with spaceborne interferometric synthetic aperture radar data (high spatial resolution) can reveal much more about the complexity of large landslide movement than is possible with geodetic measurements tied to only a few specific measurement sites. This approach is applied to an ~4 km2 reactivated tran
Authors
Xie Hu, Zhong Lu, Thomas C. Pierson, Rebecca Kramer, David L. George
By
Natural Hazards Mission Area, Landslide Hazards Program, Volcano Hazards Program, Volcano Science Center, Geologic Hazards Science Center

Volcano geodesy in the Cascade arc, USA

Experience during historical time throughout the Cascade arc and the lack of deep-seated deformation prior to the two most recent eruptions of Mount St. Helens might lead one to infer that Cascade volcanoes are generally quiescent and, specifically, show no signs of geodetic change until they are about to erupt. Several decades of geodetic data, however, tell a different story. Ground- and space-b
Authors
Michael P. Poland, Michael Lisowski, Daniel Dzurisin, Rebecca Kramer, Megan McLay, Benjamin Pauk
By
Volcano Hazards Program, Volcano Science Center

Science and Products

Combining InSAR and GPS to determine transient movement and thickness of a seasonally active low-gradient translational landslide

The combined application of continuous Global Positioning System data (high temporal resolution) with spaceborne interferometric synthetic aperture radar data (high spatial resolution) can reveal much more about the complexity of large landslide movement than is possible with geodetic measurements tied to only a few specific measurement sites. This approach is applied to an ~4 km2 reactivated tran
Authors
Xie Hu, Zhong Lu, Thomas C. Pierson, Rebecca Kramer, David L. George
By
Natural Hazards Mission Area, Landslide Hazards Program, Volcano Hazards Program, Volcano Science Center, Geologic Hazards Science Center

Volcano geodesy in the Cascade arc, USA

Experience during historical time throughout the Cascade arc and the lack of deep-seated deformation prior to the two most recent eruptions of Mount St. Helens might lead one to infer that Cascade volcanoes are generally quiescent and, specifically, show no signs of geodetic change until they are about to erupt. Several decades of geodetic data, however, tell a different story. Ground- and space-b
Authors
Michael P. Poland, Michael Lisowski, Daniel Dzurisin, Rebecca Kramer, Megan McLay, Benjamin Pauk
By
Volcano Hazards Program, Volcano Science Center
Was this page helpful?