Unit 2: Physical Geography (P1) Flashcards
What are the 4 major Geological Eras?
Cenozoic (0-65 M years ago)
Mesozoic (65 - 248 M years ago)
Palezoic (248 - 540 M years ago)
Precambrian (540 - 4500 M years ago)
Precambrian Era
[earliest life , 88% of history]
Major Geologic Events:
- Precambrian shields (eg. Canadian, Brazilian, African, and Australian Shields) are formed
Major Biological Events :
- First single-celled organisms
- First multi-celled organisms
Palezoic Era
[ancient life , 7% of history]
Major Geologic Events :
- Periods when large parts of North America are covered by shallow seas
- Appalachians formed (Northeastern North America)
Major Biological Events :
- First plants and animals appear on land
- Large swamps (Coal eventually formed from this vegetation)
- First insects
- (Age of amphibians and fish)
Mesozoic Era
[middle life , 4% of history]
Major Geologic Events:
- Shallow seas in the interior of North America at various times
- Innuitian Mountains formed (Canadian Arctic region today)
- Formation of the Rocky Mountains begins
Major Biological Events:
- First birds and mammals
- First flowering plants
- Age of reptiles, such as dinosaurs
Cenozoic Era
[recent life , about last 1% of history]
Major Geologic Events:
- Formation of the Rocky Mountains completed
- Continents take on their present shape
- Ice sheets cover much of North America
Major Biological Events :
- Modern forms of life evolve
- Human beings develop
- age of mammals
Palezoic Era is the age of….
amphibians and fish
Cenozoic Era is the age of….
mammals
Mesozoic Era is the age of….
reptiles, such as the dinosaurs
History of continental drift theory?
Alfred Wegener noticed that continents fit together like a puzzle piece + same species in diff continents
was ridiculed until more research was done to find out he was right
- thermal convection in the mantle could move the continental crust on top of it.
- When Earth’s magnetic field slips, magnetic material in the deep earth (hot magma) preserve the fingerprint (cools/hardens in2 rock), geologists can analyze rock and trace back history –seafloor was spreading apart at ridged where new rock was oozing up from the hot mantle
What is continental drift theory?
states that Earth’s continents were once joined together as a single supercontinent called Pangaea, and over time, they have gradually drifted apart to their current positions
Plate tectonics is a modern update on what earlier theory?
Continental Drift Theory
What is the mantle?
the rocky inner layer above the Earth’s core
what is the lithosphere
the Earth’s solid outer layer
Explain Convergent boundaries.
where plates collide into one another. Where those plates meet, Earth’s crust crumbles and buckles into mountain ranges. (eg: India & Asia came tg abt 55 M yrs ago 2 create the Himalaya Mountains. As the mash-up continues, those mountains grow higher and higher)
What is Subduction in relation to plate boundaries?
Converging plates don’t always collide upward. Sometimes, an ocean plate (which is made of denser rock than landmasses) collides with a continental plate, in which case it “subducts” or dives beneath the other plate. It then descends into the Earth’s mantle, the layer underneath the crust, melts in the mantle’s hot magma, and is spewed out in a volcanic eruption.
Explain Divergent boundaries.
tectonic boundaries where plates “diverge” or are tugged apart.
What is created when plates diverge under the ocean?
mid-ocean ridges
Explain Transform boundaries.
where plates move sideways in relation to each other.
Also the slip-sliding motion of plate boundaries that triggers many earthquakes.
Generally what is the rate of plate movement?
rate of one to two inches (three to five centimeters) per year, according to National Geographic
- about as fast as fingernails
What is the Ring of Fire
a path along the Pacific Ocean with a bunch of active volcanoes and frequent earthquakes
Erosional processes?
weathering, erosion, deposition
erosion?
the moving of broken-up pieces of rock.
weathering?
the breaking down of rocks.
deposition?
The building up of eroded materials in a new location.