3. ♥Deformation – the breaking, tilting, and
folding of crustal rock due to crustal
movement.
4.
5.
6.
7. Alfred Wegener (1880-1930)
• He claimed that
Earth used to have
only one supergiant
and land mass where
all continents came
from.
8. • He called this massive land
mass Pangaea
• surrounded by an ocean
mass called Panthalassa
9.
10. 2 giant continents
1. Laurasia - comprised the northern
continents of today’s times.
2. Gondwanaland - comprised the
continents in the present southern
hemisphere.
11. Eduard Suess (1831-1914)
• Recognized the existence of
Gondwanaland
• Known to have proposed the
existence of Tethys Sea, the only
recognized body of water during
those ancient times.
17. c.Lystrosaurus
• Early Triassic terrestrial mammal-like reptile
• About 1 meter long with two long teeth protruding from the upper jaw
• Fossils found in Africa, India, and Antarctica
18. d.Cynognathus
• Early Triassic terrestrial mammal-like reptile
• About 1 meter in length
• Fossils found in Brazil and Africa
28. ♥The similarity of rock layers found in
mountains that are on the opposite
sides of the Atlantic Ocean.
♥The Appalachian Mountains, Scandes
Mountains of Norway and Caledonian
Mountains of Scotland were thought
to be one mountain rage in Pangaea.
29.
30.
31. ♥The rock types found in Brazil,
India, South Africa and
Antarctica seem to have
similar layers and sequence
♥Glossopteris fossils were
found in the rock of each
continent.
32.
33.
34. “
Objectives
Find clues to solve a problem; and
Recognize how the continental Drift
Theory is developed
35.
36. 1. Do this activity in a group of
five/six.
2. Obtain a set of torn
newspaper/printed page from your
teacher.
3. Try to fit the pieces together.
37. Questions
1. What features of newspaper/printed page
helped you to connect the pieces perfectly?
2. How do lines of prints or text in the
newspaper/printed page help you to confirm
that you have reassembled the
newspaper/printed page?
38.
39. Arthur Holmes (1890-1965)
• Suggested the idea of thermal convection
as the driving force for the movement of
the continents.
• Suggested that the thermal convection
works like a “conveyor belt” where the
pressure that goes up could break apart a
continent.
40. • While the basis for the movement
of continents progresses,
geologists started to use a more
precise term to refer the moving
piece of crust as “plate” because
it is believed that continents are
not the only ones moving.
41. 7 major plates
1. Pacific Plate
2. Eurasian Plate
3. North American
Plate
4. South American
Plate
5. Indo-Australian
Plate
6. Antarctic Plate
7. African Plate
42.
43. 3 Major Types of Plate
Boundaries:
a.Divergent Plate Boundaries
b.Convergent Plate Boundaries
c.Transform Plate Boundaries
54. 1. Normal Fault – fault caused by tension
stress that moves the hanging wall down
relative to the foot wall.
55. 2. Reverse Fault – fault caused by
compression forces where the hanging
wall will move up relative to the foot wall.
56. Thrust Fault – is formed when compression
causes the hanging wall to slide over the
foot wall. (almost horizontal movement)
57. 3. Strike-slip Fault - the two blocks move either to
the left or to the right relative to one another.
Strike-slip faults are associated with crustal
shear.
63. Seafloor Spreading
Is a continuous process where
tensional forces on both sides of
the plates cause them to constantly
move apart.
Happens along Mid-oceanic ridges.