EarthScope scientists use state-of-the-art instruments and methods to collect data from seismic waves, crustal movements, Earth's magnetic field, rock and soil samples, and images obtained from aircraft and satellites. This research helps us better explain geological phenomena, protect ourselves against natural hazards, and locate necessary resources. By integrating information derived from its three multi-disciplinary observatories (US Array, PBO, and SAFOD), EarthScope aims to understand and describe how geological forces shaped North America's landscape and to contribute to the public's understanding of our dynamic Earth.
Probing Beneath the Surface
To determine how features seen at Earth's surface correlate with structural and compositional differences deep within the planet, seismologists need denser networks of seismic stations so that they are recording seismic waves that propagate through finer and finer slices of the earth beneath them. (Find out how a seismometer works.) This information will also enable scientists to link structures inherited from earlier stages of continental formation to known and potential geologic hazards (e.g., earthquakes, volcanoes, landslides).
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. The US Array is made up of four parts:
- Transportable Array: A network of 400 movable seismographs, arranged in a grid pattern approximately 70 km apart. Stations are moved west to east every two years.
- Flexible Array: An additional pool of seismic instruments that can be configured for high density, short-term observations within the larger Transportable Array.
- Reference Network: A permanent network of instruments that provides long-term comparison for observations made with the Transportable Array as it makes its way across the country.
- Magnetotelluric Array: A network of permanent and portable instruments which measure the Earth's naturally occurring electric and magnetic fields.
Therein Lies the Rub
At the simplest level, earthquakes happen when parts of Earth's crust move. But, what happens at plate boundaries is actually quite complicated. To find out just how complicated things are, the Plate Boundary Observatory (PBO) is exploring the structure and evolution of the North American continent and the processes related to earthquakes and volcanoes using an array of high precision GPS stations, borehole strainmeters, and tiltmeters positioned throughout the western United States.
Questions being addressed by PBO:
- What are the forces that drive plate-boundary deformation (small changes in length and volume)?
- 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 (begin to form)?
- What are the dynamics of magma rise, intrusion, and eruption?
- How can we reduce the hazards of earthquakes and volcanic eruptions?
No Small Task
The PBO network has a 1100
Data from PBO's integrated network of GPS stations, strainmeters and seismometers, coupled with aerial and satellite imagery, are providing important temporal constraints on plate boundary deformation and are improving our knowledge of the fundamental physics that govern deformation, faulting, and fluid transport in earth's lithosphere.
Cloudy with a Chance of Tremors?
Millions of lives are threatened every year by the potential consequences of a strong earthquake. How many of those lives could be saved if we knew when and where an earthquake was going to happen ahead of time?
Although there are currently no reliable methods for predicting the exact time, location, and magnitude of an earthquake (and there may never be), scientists are making strides toward improved "seismic weather reports," which estimate the probability of earthquakes in a given locale. By observing quakes "up close," EarthScope's San Andreas Fault Observatory at Depth (SAFOD), is contributing to a major advance in the pursuit of a rigorous scientific basis for assessing earthquake hazards and predicting earthquakes. SAFOD will directly reveal, for the first time, the physical and chemical processes controlling earthquake generation within a seismically active fault.
Instruments such as seismometers, strainmeters, pressure meters, and tilt sensors inside the borehole, along with core and fluid samples extracted during drilling, provide direct information about the physical conditions under which earthquakes occur. Scientists are using SAFOD data to learn about the:
- composition and mechanical properties of rocks in the fault zone
- nature of stresses responsible for earthquakes
- role of fluids in controlling faulting and earthquake recurrence
As part of the efforts of the National Earthquake Hazards Reduction Program, SAFOD, along with USGS and the Parkfield Earthquake Experiment, will help scientists achieve a better understanding of what happens on and near a fault during the earthquake cycle. These data will aid their ability to predict the time and severity of future quakes and to protect lives and property from the harms associated with earthquakes.