copyright 2000 Joseph Hull
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Alternative Division of Earth:
based on how Earth rocks behave mechanically
lithosphere
("rocky sphere"), includes crusts plus some upper mantle
lithosphere: outer layer, coldest and therefore strongest rocks, rigid
layer
lithosphere is strong but brittle, breaks dramatically (earthquakes...)
asthenosphere
("weak sphere"), rest of mantle below lithosphere
asthenosphere: inner layer, hottest and weakest rocks, solid but
gooey
asthenosphere is weak and gooey solid, flows like cold honey but as a solid
Plate Tectonics: movement
of plates on the surface of the Earth
plates: pieces
of lithosphere (outermost cold rigid layer of Earth)
each plate moving at own speed (1-15 cm/year) in own direction: absolute
motion
plate movement driven by solid state convection of Earth's mantle
motion of plate reflects motion of mantle + complications
present day motion of plates determined by Global Positioning Satellite
(GPS)
past motion of plates determined by hot spot tracks (e.g. Hawaiian Islands)
past motion also determined partly by ancient magnetic field of Earth
ancient magnetic field trapped in old rocks, tells original latitude
Plate Tectonics Rules (tektos:
to move around)
(1) lithosphere
divided into pieces called plates: rigid slabs of lithosphere
(2) plates are
moving around on surface of Earth!! moving a few inches per year
(3) asthenosphere
is heated from below, light asthenosphere rises as solid to surface
(4) as asthenosphere
cools and sinks, plates dragged around on surface of Earth
(5) plates grind
past, bump into and pull way from each other, creating geology!
North American Plate:
WA is currently at western/leading edge of NAM
in PNW, NAM currently
moving towards southwest about 5 cm/year
overall, NAM
currently rotating CCW about an axis somewhere off Florida
(our data base changing fast with direct measurements by GPS)
NAM has been
moving uniformly for at least the last 20 Ma
leading edge
of NAM is taking some abuse, deforming internally, not rigid
Olympics/Willapa Hills/Coast Range being pushed to NE and rotating
see this from PANGA study (Pacific Northwest Geodetic Array)
Juan de Fuca, Gorda and Explorer
Plates: all made of oceanic crust + mantle
very small plates
today. motions poorly known (no islands, no GPS)
JDF was enormous in past, called the Farallon plate
probably
moving 5 cm/year towards NE (Cobb seamount chain)
Gorda Plate may
have been/is being ripped off of JDF plate
Gorda Plate deforming internally with many quakes on many faults
therefore not obeying 1st law of plates (must be rigid internally)
Pacific Plate: nearby
to south and north of PNW; PAC is biggest plate today
moving 10-15
cm/year towards WNW, pretty uniform for a big plate
big change in
plate motion about 35 Ma ago, PAC was going N, then turned
Two Plates Interact:
diverge, converge and slide past each other sideways
motion of one
plate relative/compared to another is relative motion
NAM-JDF Relative Motion:
two plates converging about 10 cm/year NE-SW
plate boundary
called Cascadia subduction zone: JDF subducting under NAM
recycling of JDF oceanic crust into mantle beneath NAM
creates
East-dipping plane of earthquakes getting deeper to east
shallow/low angle subduction because JDF crust is still quite warm
1999 Satsop 5.5 quake most recent big one along subduction zone
creates
arc of explosive, Andean-type volcanoes (St. Helens, Rainier...)
scrapes
off sediment from JDF plate and piles it up along plate margin
JDF sliding NE
under North-South edge of NAM = oblique convergence
convergence NOT at right angles to N-S plate boundary
oblique convergence here produces Northward drag on NAM by JDF
NAM-PAC Relative Motion:
sideways/transform about 10-15 cm/year
along San Andreas
transform and Queen Charlotte transform
eventually (5-10
Ma from now) have transform in Puget Sound......
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