6. CONVERGING PLATES DIVERGING PLATES
1 MOUNTAINS 1 RIFT VALLEY
2 VOLCANOES 2 CONSTRUCTIVE
3 SUBDUCTION 3 WIDER OCEAN
4 BUMP 4 SEPARATE
5 ISLAND ARC 5 NEW OCEAN
FLOOR
6 DESTRUCTIVE 6 RIDGES
7.
8.
9. What is Transform Fault Boundary?
- two plates slide past one another
where the motion is predominantly
horizontal.
- the fracture zone that forms a
transform plate boundary is known as
transform fault.
- natural or human-made structures
that cross a transform boundary are
10. - most of the transform faults are found in
the ocean basin, few in the continental
crust
- it is a conservative type boundary , no
lithosphere is created nor destroyed,
instead, rocks are displaced, pulverized
along shearing zones as the plates grind,
creating linear fault valley or undersea
canyon.
11. At shearing zones
- shallow earthquakes happen
frequently
- massive rocks are torn apart and
displaced
tens to hundred miles away along this
area
15. RIDGE-RIDGE
- Transform faults that offset
mid-oceanic ridges ,transfer
spreading from one segment
of the ridge to the next.
16.
17.
18. RIDGE-TRENCH
- transform faults can also occur between a
spreading center and a subduction
zone (ridge-trench or ridge-arc arc transform).
- a transform fault that connects spreading
center to deep -sea trenches in subduction
zones.
25. Virgin Islands National Park is a sheared-
up landscape forming as the Carribean
plate slides eastward past the oceanic
part of North American Plate