Title: EarthScope
1- EarthScope
- Plate Boundary Observatory
2Introduction
EarthScope Revealing Earth's Secrets Jayme B.
Margolin PBO Siting Education and Outreach
Specialist margolin_at_unavco.org UNAVCO, Boulder,
Colorado February 25, 2008 Mesa Union School
3Outline
- The Plate Tectonic Theory
- Global Positioning System (GPS)
- Plate Boundary Observatory (PBO) and You
- Current Data and Science
- Geological Hazard Activity
- Conclusion
4Plate Tectonics
(from http//mediatheek.thinkquest.nl/, 2007)
5Plate Tectonics
The Theory of Plate Tectonics
(from http//en.wikipedia.org/wiki/Plate_tectonics
, 2008)
6Ring of Fire
(From www.worldbook.com, 2008)
7Plate Boundaries
Plate Tectonics
- Transform
- Divergent
- Convergent
(from USGS, 2005)
8Plate Movement
(from USGS, 2006)
9Global Positioning System (GPS) Examples
GPS Examples
10Method of Operation
- Global positioning system (GPS)
- Receiver determines location, speed, direction,
and time - 3 satellite signals are necessary to locate the
receiver in 3D space - 4th satellite is used for time accuracy
- Position calculated within sub-centimeter
11Anatomy of a GPS Station
- GPS antenna inside of dome, solidly attached into
the ground with braces. If the ground moves, the
station moves. - Solar panel for power
- Equipment enclosure
- GPS receiver
- Power/batteries
- Communications/ radio/ modem
- Data storage/ memory
12Movement of GPS stations
GPS station positions change as plates move.
How will the position of these stations change
relative to one another?
13EarthScope Partners
EarthScope is funded by the National Science
Foundation and conducted in partnership with the
US Geological Survey.
EarthScope is being constructed, operated, and
maintained as a collaborative effort with UNAVCO,
IRIS, and Stanford University, with contributions
from NASA and several other national and
international organizations.
The data collected by EarthScopes three
observatories will help us to understand
processes that control earthquakes and volcanoes.
14SAFOD
A borehole laboratory on the San Andreas fault
studying the physics of earthquake nucleation at
the depths where earthquakes begin.
15US Array
A continent-spanning deployment of seismometers
for imaging the deep interior of the North
American continent
16Transportable Array
17Plate Boundary Observatory
- A continent-scale network of GPS, borehole, and
laser strainmeters focusing on the extended plate
boundary and extending into the continental
interior - Measurements of
- Extension/compression
- Dilatation
- Tilt
18PBO Instruments
1100 Continuous GPS
103 Borehole Strainmeters and Seismometers
5 Laser Strainmeters
28 Shallow Borehole Tiltmeters
18
19GPS Monuments
GPS Station
Monument drilling
Moderate impact Deep Drill Braced
GPS Monument
Monument installation
Final site
20PBO Science Goals
- Earthquake processes and seismic hazards
- Magmatic processes and volcanic hazards
- Active deformation and tectonics
- Exploration and discovery
Requires an Interdisciplinary Approach
21Faults - Chaos
22Mesa Union Region
23Visible Results
Deformed rocks within the San Andreas Fault zone
(from J.K. Nakata, 1988)
24So. CA GPS Sites
25Mesa Union School
Local GPS Stations
Site Webpage http//pboweb.unavco.org/shared/scrip
ts/stations/?checkkeyP729
26Time Series
(from Southern California Earthquake Center, 2007)
27Vectors
28Science Example
- Producing PBO GPS
- velocity solution maps
- Supported scientist Thorsten W. Becker
(University of Southern California in Los
Angeles) - Main research interests as a geophysicist
focuses on tectonic deformation
(from http//geodynamics.usc.edu/becker, 2007)
29Science in Use
30Hazards
Hazards
In addition to seismic hazards (earthquakes) in
your region, what are some other hazards?
Tsunamis
Liquefaction
Now lets have some fun
31Summary
Determine Through Geodetic (crustal movement)
Observations of Plate Boundaries
(from mymapman.com, 2008)
(from www.scenta.co.uk, 2007)
(from noaa, 2007)
32Science
Earth Science ... from the
descriptive to the numerical
from regional to
global
33Questions?
Are there any questions, comments, or concerns?
34Useful Web Links
- www.earthscope.org
- www.unavco.org
- www.unavco.org/EO
- pboweb.unavco.org/
- www.dlese.org/library/index.jsp
- projects.crustal.ucsb.edu/understanding/
- www.DaretoPrepare.org
- www.explorers.org/
- www.nsf.gov/home/grants
- sopac.ucsd.edu/
35Extra Slides
36Educators
37Data for Educators
38Science Examples
39PBO Network Overview
- Focused, dense deployments of GPS and strain
- 775 continuous Global Positioning Systems
- 175 borehole strainmeters
- 5 long baseline strain components
- Backbone network of GPS stations
- 100 sites to provide a long-wavelength,
long-period synoptic view of the entire plate
boundary zone. Receiver spacing is approximately
200 km - 16 backbone sites in eastern US at 400 km
spacing - Portable GPS receivers
- Pool of 100 portable GPS receivers for temporary
deployments to areas not sufficiently covered by
continuous GPS