The USArray component of the NSF-funded EarthScope project ended its observational period in September 2021 and all remaining close-out tasks concluded in March 2022. Hundreds of seismic stations were transferred to other operators and continue to collect scientific observations. This website is now in an archival state and will no longer be updated. To learn more about this project and the science it continues to enable, please view publications here: and citations of the Transportable Array network DOI 10.7914/SN/TA.

To further advance geophysics support for the geophysics community, UNAVCO and IRIS are merging. The merged organization will be called EarthScope Consortium. As our science becomes more convergent, there is benefit to examining how we can support research and education as a single organization to conduct and advance cutting-edge geophysics. See our Joining Forces website for more information. The site will soon host the new EarthScope Consortium website.

A Continental-scale Seismic Observatory


USArray is a 15-year program to place a dense network of permanent and portable seismographs across the continental United States. The seismographs record local, regional, and distant (teleseismic) earthquakes.

USArray consists of four interrelated parts.

1. Transportable Array

USArray has a large traveling network of 400 high-quality, portable seismographs that are being placed in temporary sites across the United States in a rolling fashion. Station spacing is ~70 km (42 mi). Transportable Array data are extremely useful for mapping the structure of Earth's uppermost 70 km. The array was initially deployed in the westernmost United States. Unless adopted and made into a permanent installation, after 18-24 months, each instrument is picked up and moved to the next carefully spaced array location to the east. When completed, over 2000 locations will have been occupied during this program.

Transportable Array Information

2. Flexible Array

As the Transportable Array moves across the country, a pool of hundreds of additional portable seismometers is available to scientists for dispatching to specific targets for more detailed studies. These instruments might be set up, for example, to chart the magma chamber beneath Yellowstone, or to map the geologic structure deep beneath New Madrid, Missouri, to understand why big earthquakes occurred in the region. If these targeted arrays are placed in seismically quiet areas, scientists can use manmade vibrations produced, for example, by explosives in a drill hole or by a large ground-tamping truck, to cause ground motion that can be recorded by the seismic sensors. Even random, "cultural" noise can be used to image the earth. The dense instrument coverage enabled by the Flexible Array can be used map, in much greater detail, specific structures that are in the upper 70 km of the earth.

Flexible Array Information

3. Reference Network

USArray, in close collaboration with the US Geological Survey's Advanced National Seismic System (ANSS) has contributed to the establishment of a permanent network of seismic stations across the United States with uniform spacing of approximately 300 km (186 mi). The Reference Network provides the baseline measurements for the Transportable Array and Flexible Array.

Reference Network Information

4. Magnetotelluric Facility

EarthScope is installing a small number of permanent and portable magnetotelluric (MT) sensors across the United States in conjunction with USArray seismic instrumentation. These MT sensors record naturally occurring electric and magnetic fields, which scientists will integrate with other geophysical data to identify Earth's thermal structure and to study the significance of fluids within Earth's lithosphere (upper ~70 km). An MT station is passive with no associated noise or motion, and consists of a magnetometer, four electrodes, and a data-recording unit that are buried in shallow holes. The four electrodes are placed along two lines in a cross or "L" shape, oriented along north-south and east-west directions, and connected by a thin cable to the magnetometer and data recording unit which are usually at the intersection of the two lines. The electrodes are saturated with a common salt solution to improve conductivity with the ground.

Magnetotelluric Facility Information