Using GPS to monitor tectonic plate motions across the San Andreas fault in southern California...
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Using GPS to monitor tectonic plate motions across the San Andreas fault in southern California Sally McGill California State University, San Bernardino This material is based upon work supported by the National Science Foundation under Grant Number 0844400. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science
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Transcript of Using GPS to monitor tectonic plate motions across the San Andreas fault in southern California...
Using GPS to monitor tectonic plate motions across the San Andreas fault in
southern California
Sally McGillCalifornia State University, San Bernardino
This material is based upon work supported by the National Science Foundation under Grant Number 0844400. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.
• Note to teachers: • I generally introduce this lesson with a review
of plate tectonics including:– The three types of plate boundaries and the types
of motion associate with each– A world map of the ocean floors or a world map of
tectonic plates, on which I point out that the Pacific Plate • is created at a mid-ocean ridge in the southeastern
Pacific ocean• It travels northwestward until it is consumed at
subduction zones off the coasts of Alaska, Japan, etc.• And along the way it slides horizontally past California,
which is why we have a transform plate boundary in California.
Pacific-North American Plate Boundary
What type of motion occurs along the San Andreas fault?
Pacific-North American Plate Boundary
What direction is the Pacific Plate moving relative to North America?
Pacific-North American Plate Boundary
What direction is the Pacific Plate moving relative to North America?Toward the northwest
How do we know?
P612
Global Positioning System (GPS).
Portable GPS antenna mounted on a tripod and centered exactly over a benchmark
NORCO
6106
ARROWHEAD
MT. LUNA
POINT65OakHillsH.S.
San BernardinoMountains
NORCO
6106
ARROWHEAD
MT. LUNA
POINT65OakHillsH.S.
Sites on the North American Plate:
Sites on the Pacific Plate:
San BernardinoMountains
Active Faults of Southern California
NORCO
6106
ARROWHEAD
MT. LUNA
POINT65OakHillsH.S.
Which site do you expect to be moving the fastest (relative to the North American Plate)?
The slowest?
NORTH AMERICAN PLATE
PACIFICPLATE
San BernardinoMountains
Site--POINT65
Date North position (cm) East position (cm)1993.6 0.00 0.001995.6 3.40 -5.921999.8 9.01 -10.442002.5 13.80 -16.622002.9 14.39 -16.732003.5 14.92 -16.762004.5 16.72 -18.882005.5 17.36 -20.302007.8 20.51 -22.642008.5 21.35 -23.792009.6 22.89 -24.662010.5 23.83 -25.97
POINT65--North
0.00
5.00
10.00
15.00
20.00
25.00
30.00
1990 1995 2000 2005 2010 2015
Year
Nor
th p
ositi
on (c
m)
POINT65--East
-30.00
-25.00
-20.00
-15.00
-10.00
-5.00
0.00
1990 1995 2000 2005 2010 2015
Year
East
pos
ition
(cm
)
Demonstrate how to plot the north and east positions as a function of time.
Site--POINT65
Date North position (cm) East position (cm)1993.6 0.00 0.001995.6 3.40 -5.921999.8 9.01 -10.442002.5 13.80 -16.622002.9 14.39 -16.732003.5 14.92 -16.762004.5 16.72 -18.882005.5 17.36 -20.302007.8 20.51 -22.642008.5 21.35 -23.792009.6 22.89 -24.662010.5 23.83 -25.97
POINT65--North y = 1.408x - 2806.3
R2 = 0.9959
0.00
5.00
10.00
15.00
20.00
25.00
30.00
1990 1995 2000 2005 2010 2015
Year
Nor
th p
ositi
on (c
m)
POINT65--East y = -1.4759x + 2940.4
R2 = 0.9828
-30.00
-25.00
-20.00
-15.00
-10.00
-5.00
0.00
1990 1995 2000 2005 2010 2015
Year
East
pos
ition
(cm
)
NORCO
6106
ARROWHEAD
MT. LUNA
POINT65OakHillsH.S.
Which site is actually moving the fastest (relative to the North American Plate)?
The slowest?
NORTH AMERICAN PLATE
PACIFICPLATE
1.6 cm/yr
1.7 cm/yr
2.4 cm/yr
3.0 cm/yr3.3 cm/yr
Elastic Rebound
1. A road is constructed across the fault shortly after stress on the fault has been released by the previous earthquake.
Elastic Rebound2a. During the following decades or
centuries, the tectonic plates on which the road is built continue to move even though the fault itself is locked by friction and is not slipping at the surface or in the upper part of the Earth's crust. This causes the plates to bend elastically within 10-20 km on either side of the fault. The more the plates bend, the more the shear stress builds up on the fault.
Elastic Rebound
2b. We can use GPS to measure how fast the plates are bending. The blue arrows illustrate the speed and direction of motion of survey benchmarks located in a line across the fault. Note that during this interseismic period (in between earthquakes) the velocities of the stations change gradually, rather than abruptly, across the fault.
Elastic Rebound
3. Eventually the shear stress on the fault becomes stronger than the friction that is keeping the fault stuck, and the two sides of the fault suddenly slide past each other, resulting an earthquake. After the earthquake we can see an abrupt shift in the road across the fault, and the road is no longer bent.
NORCO
6106
ARROWHEAD
MT. LUNA
POINT65OakHillsH.S.
Which site is actually moving the fastest (relative to the North American Plate)?
The slowest?
NORTH AMERICAN PLATE
PACIFICPLATE
1.6 cm/yr
1.7 cm/yr
2.4 cm/yr
3.0 cm/yr3.3 cm/yr
