džiomorfolodži Flashcards

(45 cards)

1
Q

Layers (4)

A

Crust
Mantle
Outer & Inner Core

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2
Q

Lithosphere

A

Crust + Upper part of Mantle

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3
Q

Asthenosphere

A

Part of upper Mantle below Lithosphere
Flows like molten plastic despite being solid

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4
Q

Outer Core

A

Fluid layer of Earth’s Core
Primarily composed of Liquid Iron & Nickel
4500C to 5500C
2900km to 5100km

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5
Q

Inner Core

A

5100km to 6371km from surface
Probably: solid, composed by iron-nickel alloy
->deduced from seismic waves & magnetic field

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6
Q

Tectonic plates boundaries (3)

A

Divergent, Convergent, Transform

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7
Q

Divergent boundary - Separation

A

Plates move away from each other
New crust
Under oceans usually (basalt)
Mid-Atlantic Ridge
East African Rift Valley
Constructive

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8
Q

Convergent boundary - collision

A

Causes: Subduction OR Collision
Creates mountains
Subduction - usually oceanic going under continental
Destructive

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9
Q

Transform (Sliding)

A

Plates slide past each other horizontally
Causes Earthquakes
E.g.: San Andreas Fault

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10
Q

Convergent - results

A

Mountains, Trenches, Volcanoes

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11
Q

Divergent - results

A

Ridges, Valleys

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12
Q

Transform - results

A

Earthquakes, faults

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13
Q

Fault

A

Break or fracture of Earth’s crust where rocks have moved past each other
Cause: tectonics forces that are too strong, causing rocks to crack and shift
Result: Displacement: up/down/sideways

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14
Q

Mohorovicic Discontinuity/Moho

A

Seismic waves change speed as they move
Speeding up when pass through bottom of crust enter mantle
Boundary between crust and upper mantle

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15
Q

Desulforudis Audaxviator

A

Species of bacterium that lives in groundwater 1.5-3km below Earth’s surface
Jules Verne’s novel Journey to the Center of the Earth: “Descende, audax viator, et terrestre centrum attinges”

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16
Q

Magnetic Motion

A

Earth’s north magnetic pole is moving away from Canada toward Siberia

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17
Q

Folds

A

Bend in rock layers caused by slow compression
Cause: Rock layers are soft/flexible, pressure applied slowly, so they bend instead of breaking
Result: Curved structures: Anticlines(upfolds)/Synclines(downfolds)

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18
Q

Convection Currents

A

Circular movements of material caused by differences in temperature/density in Earth’s mantle

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19
Q

Convection Current process (technically 4 but 5)

A
  1. Heat from Core warms lower mantle
  2. Hot mantle material becomes less dense and ascends
  3. Reaching cooler upper mantle makes it spread out and cool down
  4. Cooler and denser material sinks back toward lower mantle
  5. Cycle…
20
Q

Mantle Plume

A
  1. Narrow column of hot rock that rises deep within the mantle, possibly near Core
  2. Hotter & more buoyant than surroundings, causing it to rise vertically and drastically
  3. When it reaches lithosphere, it can cause volcanic activity(e.g. Hawaii Islands formed over a mantle plume - hot spot)
21
Q

Hot Spot

A

Usually away from boundaries
Caused by Mantle Plumes

22
Q

Ring of Fire

A

Location: Around Pacific Plate edges
Cause: Convergent plate boundary = Subduction
Definition: Zone of intense volcanic and earthquake activity

23
Q

Continental crust

A

thicker/stronger 35-40km
older
less dense
mostly granite

24
Q

Oceanic crust

A

slightly denser
much thinner 5-10km
younger
mostly basalt

25
Causes of plates movement
Convection Currents Force of Gravity Weight of plate
26
Old continents
Pangea ->Laurasia+Gondwana
27
Old Seas/Oceans
Panthalassa Tethys
28
Eons
Phanerozoic 541Ma Precambrian: -Proterozoic 2.5Ga -Archean - 4.0Ga -Hadean - 4.54Ga
29
Phanerozoic Eon - Eras
Cenozoic - 66Ma Mesozoic - 252Ma Paleozoic - 541Ma
30
Paleozoic periods (8 fancy worte ;))
1. Cambrian - 541Ma 2. Ordovician 3. Silurian 4. Devonian 5. Carboniferous: 5.1 ->Mississippian 5.2 ->Pennsylvanian 6. Permian - end 252Ma
31
Mesozoic (3)
1. Triassic - 252Ma 2. Jurassic 3. Cretaceous - 66Ma
32
Cenozoic (3 periods)
Paleogene Neogene Quarternary
33
Epoch
Paleogene: 1. Paleocene 2. Eocene 3. Oligocene Neogene: 1. Miocene 2. Pliocene Quarternary: 1. Pleistocene 2. Holocene - since 11.8Ka
34
Cratons
Old and Strong part of continental plate
35
Platform
craton covered with sediments
36
Shield
Large area where Precambrian rocks crop out extensively at the surface
37
Acasta Gneiss
Earth's oldest known rock 4.03b years Canadian shield
38
Gneiss
metamorphic rock
39
Importance of tectonic plates movement
1. Counterbalance to erosion 2. Cooling down the Earth
40
Erosion
1. smoothening Earth's surface 2. Destroying Mountains and moving material to lowlands
41
Relief of Ocean Basins
1. Continental shelf(part of continental crust) 2. Continental slope 3. Ocean ridges 4. Ocean trenches 5. Island Arcs 6. Abyssal plain (3-6km) 7. average ocean depth = 3.7km
42
Relief on Earth (6)
Mountain Valley Hill Plateau Plain Basin
43
Formation of Relief - Internal Factors
movements inside Earth cause lithosphere to: rise, sink or move Ways: Folding & Fracturing the land Volcanoes Earthquakes
44
External Factors - Weathering, Erosion, Deposition
Erosion process Erosive agents can mould relief previously created by internal movement of the Earth Factors: 1. water -> temperature changes 2. ice 3. wind 4. vegetation 5. human actions
45
Erosion types
River carving a valley Waves cutting back cliffs Wind blowing topsoil Glacier moving rocks Landslide