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Evidence for Movement of Continents
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Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Dec 19, 2015

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Page 1: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Evidence for Movement of Continents

Page 2: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Biggest obstacles to acceptance

• You can not see the continent move

• You can not feel the motion of the continent

• Yet a lot of physical evidence supports the idea that the continents move across the earth over time

Page 3: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Goal for this section

• Review the evidence that supports continental drift

• Understand the process that allows continents to move (theory of plate tectonics)

• Predict what happens to continents and the life on them as they move

Page 4: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Question

• What kind of physical evidence could be used to show that continents move?

Page 5: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Alfred Wegener

Page 6: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Alfred Wegener

• First proposed that continents move over time (continental drift) in early 20th century

• Meteorologist and German (what effect on acceptance of his ideas did his background have)

• Could not explain how continents move, led to rejection of theory

Page 7: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Evidence for continental drift

1) Physical shape of continents

2) Rock evidence of change in climate

3) Fossil evidence, including Mesosaurus

4) Location of volcanoes and earthquakes

5) Difference in ages of oceanic crust vs continental crust. Relate age to plate boundaries

6) Magnetic orientation of rock on either side of the Mid Atlantic ridge

Page 8: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Shape of the continents

Page 9: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 10: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Pangaea and Panthalassa

Page 11: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Pangea or Pangaea

• Pangaea- name of supercontinent the last time the continents were joined

• Panthalassa- name of the single ocean that existed at the same time as Pangaea

Page 12: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Evidence for movement of continents

Page 13: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Fossil evidence

Page 14: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

• Different animals and plants require certain climate conditions to live

• When the fossils found do not match current climate…

• How did the climate change so much?

Page 15: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Fossils of ferns found in Antarctica

Page 16: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Mesosauras

• Small aquatic reptile• Less than 3 ft long• Breathed air• Freshwater hunter• Fossils found only in

eastern South America and western Africa

Page 17: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

The mystery

• In the 1800s, scientists began finding fossils of these ancient reptiles, which had long since become extinct. These fossils were found in only two regions, southern Africa and the southern part of South America. The shaded areas on the map show where fossils of Mesosaurus have been discovered. This distribution is a curious one—only two regions far from each other and separated by the Atlantic Ocean.

• What could explain this distribution?

Page 18: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

From experience with modern plants and land animal

• Migrate and expand primarily over land, not oceans.

How can the exact same land animal or plant species have existed on a number of unconnected continents ?

Page 19: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Possible answers

• Either the animals evolved the same all over the world (not consistent with recent evolution)

• Or

• The places were connected and closer in the past

Page 20: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Paper Exercise

Use the fossil evidence of shown to reassemble a supercontinent made from South America, Africa, Antarctica, India and Austraila

1. Remember, all regions of the same fossil must connect

2. It is ok to slightly overlap continents3. Glue final answer in your comp book

Page 21: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 22: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 23: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

point of exercise

Areas where fossils of land animals/plants located must be connected

This is possible only if Continents can move

Page 24: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Microfossils

• Very small life forms, organic matter

• Diatoms in ocean• Algae, pollen on land

• Localized• Quick evolution

Page 25: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Rock evidence

Rock Type indicate climate

Change in climate suggest requires change

Page 26: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Coal

• Made from organic remains of vast jungle swamps

• Indicates a tropical environment

Page 27: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 28: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 29: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Gypsum

• Created from what remains after ocean water has completely evaporated

• Indicates a hot, dry environment

Page 30: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Rock Evidence for glaciers

• Deposits made up of rocks with different size, composition, and roughness

Page 31: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Evidence of Glaciers

• Striations

Page 32: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 33: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Location of volcanoes and earthquakes around the world

Page 34: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

World Volcanoes

Page 35: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

World Earthquakes

Page 36: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Volcanoes (triangles) Earthquakes (circles)

Page 37: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 38: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 39: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Location of volcanoes and Earthquakes

• Volcanoes and earthquake line up, not randomly placed around the world

• Something must be happening on a global scale to account for this match

Page 40: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Difference in the maximum ages of ocean and continental rocks

• Max Oceanic Rock: 180 million Years old

• Max Continental Rock: over 4 Billion years old

• If continents did not move, both types should have similar ages

Page 41: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Age of the sea floor

• Red = young• Blue = old

• Connect lines created by earthquakes to ages

Page 42: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 43: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

• Oldest Oceanic crust is farthest away from the ocean ridges

• Newest Oceanic rock is found at the oceanic ridges

Page 44: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Location of world’s Oldest rocks

Page 45: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Question

• We have fossil evidence that oceans have been around for longer than 180 million years

• It was destroyed by a continuing process- suggests motion of ocean crust

Page 46: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 47: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Paleomagnetism

Page 48: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Paleomagnetism

• Study of the Earth’s magnetic record over time

• Many rocks contain magnetic minerals

• When these rocks are hot, the magnetic orientation of the minerals are random

• As they cools, the magnetic orientation of the minerals is fixed in the direction of the magnetic field of earth

Page 49: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

What is magnetic orientation?

Means the direction the compass points when moving over the rock

Page 50: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Surprising Data

• Some rocks have a magnetic orientation different from the orientation of Earth

• In the 1960’s researchers mapping the orientation of rock across the Mid Atlantic ridge found a strangely symmetric result

Page 51: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

Different colors represent rocks with different magnetic orientation

Page 52: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 53: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 54: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.
Page 55: Evidence for Movement of Continents. Biggest obstacles to acceptance You can not see the continent move You can not feel the motion of the continent Yet.

What has been discovered…

Discovered bands of rock with different magnetic orientation as the ship moves away from ridge

• Evidence that the orientation reverses every 200,000 to several million years

• Matched bands with the same magnetic orientation are found on both sides of a ridge