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Covering western North America and Alaska, EarthScope's network of high precision Global Positioning Systems (GPS) and Strainmeter stations will measure deformation across the active boundary between the Pacific and North American plates.

EarthScope Observatories


SAFOD
PBO
USArray

PBO Project Pages

UNAVCO - PBO Facility
Available online @ UNAVCO


Instrument Data

GPS Archive Data
Available online @ UNAVCO

Strainmeter Archive Data
Available online @ UNAVCO, IRIS, and NCEDC

Seismic Archive Data
Available online @ IRIS


Data Products

Raw Data Products
Available online @ UNAVCO

Processed Data Products
Available online @ UNAVCO.

Map Image of Plate Boundary Observatory Stataion Locations

The Plate Boundary Observatory (PBO) component of EarthScope is a geodetic observatory designed to study the three-dimensional strain field resulting from deformation across the active boundary zone between the Pacific and North American plates in the western United States.


More Info

The PBO mission is to site, recon, permit, install, and maintain 852 GPS, 103 borehole strainmeters (BSM), and 5 laser strainmeters (LSM) on-schedule, on-budget, and to specification within 5 years. Taken together, these instrument types span the broad temporal and spatial spectrum of plate boundary deformation anticipated in the project area. The geodetic focus of the Plate Boundary Observatory will address the following scientific questions:

  •  ›  What are the forces that drive plate-boundary deformation?
  •  ›  What determines the spatial distribution of plate-boundary deformation?
  •  ›  How has plate-boundary deformation evolved?
  •  ›  What controls the space-time pattern of earthquake occurrence?
  •  ›  How do earthquakes nucleate?
  •  ›  What are the dynamics of magma rise, intrusion, and eruption?
  •  ›  How can we reduce the hazards of earthquakes and volcanic eruptions?

GPS measures millimeter-scale ground movement on time scales of days to decades and over large spatial scales.

Borehole strainmeters measure strain change by sensing changes in the shape of an instrument cemented into rock. They play a central role in observing the deformation that accompanies and precedes earthquakes and volcanic eruptions.

Long-baseline laser strainmeters measure the change in distance between two points several hundred meters apart on the Earth's surface. Laser strainmeters have the high resolution of the borehole strainmeters combined with the long-term stability of GPS measurements.