Lesson 2 Flashcards

1
Q

What did James Ussher

A
  • used the Bible to predict the beginning of Earth
  • said Earth had a beginning date at 9 am on 4004 BC
  • to the Christian imagination, the Earth was 6000 BC
  • > mountains were made on the third day
  • > the same that that the polar zones are frozen and the tropics were warmed
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2
Q

Who is Thomas Burnet

A
  • did not think biblical explanations accounted for the creation of the World
  • > did not believe the Great Flood of the Bible accounted for the creation of the World
  • sets forth his theory of the Mundane Egg
  • > immediately after creation, the Earth was unblemished without hills
  • > it was flawless in appearance and uniform in texture
  • > it had a complicated inner structure, the fiery core(yolk)
  • > the white of the egg is the water filled abyss onto which the shell floated
  • for Burnett, the action of the Sun cracked out the Earth’s crust, letting water come out of the crust
  • > the water ripped out onto the world and caused massive floods

-his book was the The sacred theory of the Earth

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3
Q

What did Georges Buffon estimate the Earth to be

A
  • 75,000 years ago
  • > but even he said that was conservative
  • he turned each of the seven Biblical days of creation into an epoch of indefinite length
  • > created the space and time necessary for geologists to begin their work of exposing a deep history for the Earth
  • > all the while staying within the bounds of Biblical scripture
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4
Q

What was the two schools of thinking for geologists at the beginning of the eighteen hundredths

A

Catastrophism

  • > history of the Earth was dominated by major geological revolutions
  • > eg; ice, fire, comets, earthquakes
  • > drastic tidal waves, global tsunamis, severe earthquakes and volcanos, the passing of comets shaped the earth surface into its present disruption

Uniformitarianism

  • > the Earth has not had a global catostrophy
  • > earthquakes yes, volcanoes yes
  • > the change was there but the change was slow
  • > did not happy over night
  • > these phenomena like earthquakes and volcanoes rearranged the Earth within their own vicinity
  • > “the present is the key to the past”
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5
Q

What was the Grand Tour and who was the chaperone for it

A
  • it was one of the earliest forms of modern tourism from the 17 th and 18 th century
  • > it was a rite of passage for many young English and European elites to polish off their formal education by exposing themselves to continental architecture and to geography, history and culture
  • > the tour required a crossing of the European Alps

-Burnet was the chaperone for the Grand Tour

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6
Q

What the biblical key to the Earth’s appearance

A
  • it was the Great Flood
  • > a biblical story of a flood so great that it destroyed civilization
  • > but where on Earth could all that water come from
  • Burnet concluded that it would take 8 oceans of water
  • > a mere 40 days of rain, as it says in the Genesis, could hardly provide enough water to even lap at the feet of most mountains
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7
Q

Who wrote the Principles of Geology

A
  • Charles Lyell did

- >he was a Scottish geologist

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8
Q

What is so special about the Burgess Shale

A
  • this is the site of the world’s first protected complex marine ecosystem
  • > it is part of the Canadian Rocky Mountain Parks World Heritage Site
  • > remnants of an ancient sea floor can still be found among the highest peaks
  • most fossil deposits in the world preserve hard parts of animals like shells and bones and teeth
  • > the Burgess Shale preserves the soft tissues of organisms
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9
Q

What was Wegener’s contributions to the theory of mountains

A
  • he said continents move
  • he also believed that the continents were all part of one continent, named Pangaea at one point in time
  • for proof, Wegener said that the continents fit together like a jigsaw puzzle
  • > he also had proof of comparative fossil specimens and climactic evidence
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10
Q

When was Wegener’s theory of continental drift recognized

A
  • in the 1950’s

- >with advances in the study of Earth’s magnetic field

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11
Q

What is the basis of plate tectonics on Eath

A
  • that the Earth’s surface is broken up into several rigid plates
  • > these plates are made up of the Earth’s crust and the upper part of the mantle layer underneath
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12
Q

What is the litrosphere

A
  • the crust and the upper mantle are called the litrosphere

- plates gilde on the more ductile asthenosphere

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13
Q

What are the two kinds of crust are the litrospheric plates comprised of

A

-they are comprised of either continental or oceanic crust or both

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14
Q

How do ocean plates compare to continental plates

A
  • ocean plates are thinner
  • > often less than 100 km thick
  • > but they are denser than continental plates

-continental plates are roughly 150 km to 200 km thick

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15
Q

At what rate do plates move

A
  • each plate moves in various direction at rates of one to ten centimeters per year
  • > the driving force behind the slow, relentless movement is the convection in the mantle
  • > hot material near the Earth’s core rises and cold mantle rock sinks
  • where the plates pull apart, new volcanic materials fill the void
  • > hot magma wells up at these divergent plate boundaries, forming new crust and further shoving the plates apart
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16
Q

What is the largest and best known undersea mountain range

A
  • it is the Mid Atlantic Ridge
  • > which extends north/south for several thousand kilometers
  • > this is roughly parallel to the coastlines of Europe, Africa and the Americas
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17
Q

What is an example of an active continental rift zone

A
  • it is the East African Rift
  • > here the African plate is actually in the process of splitting in two
  • > as extension continues, litrospheric rupture will soon occur
18
Q

What happens when an ocean plate collides with a continental plate

A
  • the denser ocean plate is pushed or subducted beneath the more buoyant continental plate
  • > then the ocean plate is absorbed back into the hot inner earth
  • > through this process, erupting and building volcanoes can arise along the plate margins
  • note much of the Pacific Ocean boundary is surrounded by long stretches of volcanoes caused by tectonic collision
  • > this particular boundary is known collectively as the Pacific Ring of Fire
19
Q

What happens if you have two continental plates collide and it’s not as easy for one plate to subduct beneath another

A
  • in this case, the resulting collision can form the largest of mountain ranges
  • > a great example of this is the Himalaya
  • > here the Indian subcontinent is moving north into the Eurasian Plate
20
Q

What is a transform margin

A
  • these margins mark the slip sliding plates
  • > such as the San Andreas Fault
  • > where the North American and Pacific plates grind past each other in a mostly horizontal motion
  • although the forces aren’t as great here, these boundaries can still give rise to mountains on occasion
  • > such as the San Gabriel Mountains
21
Q

What are the four types of mountains

A

1) Volcanic Mountains
2) Convergent Mountains
3) Fault-block mountains
4) Dome Mountains

22
Q

How are volcanic mountains formed

A
  • they are formed when gas-rich molten rock or magma from deep within the Earth move forcefully to the surface, erupts and accumulates
  • > these rocks cool in various sizes and forms
23
Q

What is magma

A

-lava that breaks through the Earth’s crust

24
Q

What are the three basic tectonic regions that volcanoes are associated with

A
  • they are associated with rift-valley spreading centers(Iceland)
  • > or Mount Kilimanjaro on the east Africa rift system
  • also associated with convergent boundaries
  • > where one plate is subducting beneath another
  • > like Mount Fuji
  • volcanoes can also be found above intraplate hotspots
  • > where plumes of solid, yet mobile mantle rock, rise to the surface
25
Q

Why is hotspot volcanism unique

A
  • it occurs within tectonic plates
  • > and is generally not related to plate boundaries
  • > the plume that feeds the hotspot volcanos remains stationary relative to the mantle and the crust
  • > but above is always in motion
  • > a chain of regressively older volcanoes is created on the overlying plate
26
Q

Does Hawaii overlie a hotspot

A
  • yes

- >Hawaiian Islands are hotspot tracks

27
Q

Is convergent mountain the most common type of mountain

A
  • yes
  • > in fact the world’s largest mountain ranges are all convergent
  • > eg; Himalaya, Andes and European Alps
  • > these mountains are active origins, as the processes that built them are still ongoing
  • > in contrast, the Rocky Mountains of western North America and their eastern continental cousins, Appalachians are no longer active
28
Q

What happens when the plates and the continents riding on them collide

A
  • the continental crust is too buoyant to be subducted
  • > it ends up being shortened instead
  • > the accumulated layers of rocks crumple, fold and fault causing extaordinary uplift
29
Q

Where does much of the folding occur

A
  • it occurs underground

- >where the rock is hot enough to become more flexible

30
Q

What is a syncline

A
  • it is a fold
  • > where a younger rock is in the middle
  • > between layers of older rock that have been uplifted on either side
31
Q

What are anticlines

A

-folds where older rock have been brought up the middle are called anticlines

32
Q

What does the term recumbent mean

A

-syncline and anticline lying on its side is said to be recumbent

33
Q

What is a thrust fault

A
  • a gently sloping fault

- >where originally lower older rock have been pushed over younger higher rocks

34
Q

What does it mean to say that thrust faults are imbricate

A
  • they have stacked slabs of rock

- >like overlapping shingles

35
Q

When did the crust in the Appalachians begin deforming. Also describing the events leading up to Pangea

A
  • around 419 million years ago
  • > when an ancient ocean that lay to the east began to close due to the plate tectonic process of subduction
  • subduction continued until a second continent(roughly equivalent to Europe) collided with ancient North America
  • > this happened about 430 million years ago
  • > about a hundred years later, a third enormous continent, Gondwana, collided with North America
  • > by this point most of Earth’s continental crust formed a single super continent Pangea which had huge range of mountains
36
Q

When did plate tectonics tear Pangea apart? How did this affect the Appalachain mountains

A
  • plate tectonics eventually tore Pangea apart starting in the Jurassic period(118 million years ago)
  • > part of the mountain range got left behind in North America as the Appalachians
  • > other pieces got left in Scotland, Norway and Greenland
37
Q

What are fault-block mountains

A
  • they form when the faults in the Earth’s crust allow portions of the surface to drop
  • > other portions rise as opposed to Earth folding over and bending under pressure and heat
  • > eg; The Teton Range in the American Rocky Mountains
38
Q

Describe the formation of the Teton Range

A
  • less than 10 million years ago
  • > the Earth’s crust cracked or faulted
  • > west of the fault line, a block of rock about 40 km long tilted upwards to form the Teton Range
  • > east of the fault line, a block fell to form the valley called Jackson Hole
  • > with one swinging up, the other swung down

-note this fault was caused by a swelling of the Earth’s crust, not far below

39
Q

What are dome mountains

A
  • dome mountains are the result of a great amount of magma pushing itself up under the Earth’s crust
  • > without actually erupting onto the surface,the molten rock pushes out the overlaying rock layers
  • the rock layers over the hardened magma are warped upwards to form the dome
  • > while the rock layers of the surrounding area remain flat
  • > in some cases, over long periods of time, erosion can wipe away the outer layers of the mountain
  • > exposing the dome shaped cool magma now hard rock
40
Q

Give an example of a dome mountain

A
  • near the Alberta- Montana Border
  • > the formation of West Butte in the Sweetgrass Hills
  • > it formed around 48 million years ago when molten rock welled up deep within the Earth
  • > molten rock uplifted the surface sedmientary layers
  • > but solidified before reaching the surface