| Activity 1: Transform Faults and Fracture
Zones |
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Plate motions at midocean ridges are relatively
simple; i.e.,
plates move away
from the ridges as
new crust is created. In contrast, the behavior of plates at transform faults is much more complex. Recognition of the nature of this motion marked an important
development in
the theory of plate tectonics.
 However, a closer
examination of
the midocean ridge system shows that ridges are offset by a series of linear steps (Fig. 1).
These offsets or transform faults occur when the ridge first opens and do not get any longer with time. Along transform
faults, the two
lithospheric plates move past each other in opposite directions, producing shallow-level
earthquakes (Fig. 2). |
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Fig. 1: The midocean ridge system and some of its many transform faults.
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Linear structures, fracture
zones, extend out from the transform faults and past the ridges into the
ocean basins. Because
they are outside the zone of sea-floor spreading, plates on either side of a
fracture zone
move at the same rate (Fig. 2). Thus fracture zones are aseismic, lacking earthquakes, but there is a
significant difference
in age of the
ocean floor across fracture zones. Fracture zones are often characterized by steep
scarps that
provide a means
of sampling the deeper section of the ocean floor. |
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A simple paper model
elegantly illustrates
the important mechanics of transform faults and fracture zones. More... |
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| To complete Activity 1,
select one of these files: |  |  |
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