1a Evidence For Continental Drift And Plate Tectonics Flashcards
Mohorovičić discontinuity
Boundary between earths crust and the mantle
Lithosphere
Crust and upper mantle
How hot is the core
6500 degree
How hot is the mantle
1600 degrees
Density of oceanic plate
3gcm-3
Density of continental crust
2.7gcm-3
Jigsaw fit
Similarity in coastline of eastern SouthAmerica and West Africa.
Best matched 1,000 meters below sea level
Some disparities due to erosion and deposition since continental separation; eustatic and isostatic change
Geological fit
Eastern South America and West Africa have an ancient craton (2 billion years old) which continues from one content to another
Tectonic fit
Fragment of fold mountains (450 and 400 million years ago) are found on widely separated continents today
Sections of Caledonian fold mountain belt found n Ireland, Canada, Great Britain and Scandinavia . When re assembled the belt form a continuous linear feature
Glacial deposits and striations
Glacial deposit fund in Antarctica, Africa, South America, India and Australia from 300 millions years ago.
Suggesting an ice sheet covered these areas uniformly
Glacial striations (scratches on bedrock from glacier movements) show direction of ice flow from a single point
Fossil evidence
Mesosaurus remains on South Africa and EASTern South America.
Glossopteris (plant) found in Southern India, South America, Africa, Antarctica and Australia showing they were once joined
Sonar
Echo sounding bathymetry to map ocean floor
Discovered mid ocean ridges raised 1.5km above abyssal plain.
Found deepest parts ocean are close to continental margins
Provided evidence for sea floor spreading due to ridge push
Paleomagnetism
As sea floor spreads there are bands of normal polarity and reversed polarity. The symmetry and age of the rock also helped prove spreading from a single point
Sea floor spreading as part of plate tectonic theory
Seismic profiling
Provided detail about sea bed composition: only oceanic rock, not continental
Thicker sediment further from the mid ocean ridge shows it has more time to accumulate so this rock is older.
sediment cores
from ocean drilling programme
use carbon dating and dredging
rocks further from mid ocean ridge had more sediment and were older
dredged rocks from ocean floor included only basalt, gabbro and serpentinite - no continental materials