earth science Flashcards

1
Q

a geologic process in which tectonic plates—large slabs of Earth’s lithosphere—split apart from each other.

A

Seafloor Spreading

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2
Q

is a geologic process that occurs at the boundary between two plates where molten material within the earth pushes its way up, causing the plates to move away from each other.

A

Seafloor Spreading

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3
Q

A slow and steady movements of the Earth’s crust under the sea ridges

A

Seafloor Spreading

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4
Q

· Hot dense material below the Earth’s crust rises towards the mid-ocean ridge

· This materials lows sideways carrying the seafloor away from the ridge, and creates a crack in the crust

· The magma flows out of the crack, cools down and becomes the new seafloor

· Overtime, the new oceanic crust pushed oceanic crust far from the ridge and subducted

A

seafloor spreading theory

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5
Q

-is a seafloor mountain system formed by plate tectonics

A

Mid Ocean Ridge

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6
Q

examples of mid ocean ridge

A

e.g. Mid-Atlantic Ridge

East Pacific Rise

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7
Q

· He discovered seafloor spreading by using sonar.

· He first discovered seafloor spreading in early 1960s, During World War II

· He is an American geologist & US Navy officer in World War II

· He is considered as the “Founding Father” of unifying of plate tectonics

A

Harry Hammond Hess (1906-1969)

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8
Q

provides the approximate age of rocks. ________ uses the process of radioactive decay to determine the age of rocks. Using this process, radioactive elements decay at known rates to stable end products. If the percentage of stable product is known, then an approximate age can be determined. Therefore, what oceanographers did was they took samples of the seafloor and used radiometric dating to determine the age of rocks from seafloor spreading centers outwards. They discovered the age of the seafloor mirrored each other on either side of the seafloor spreading center.

A

Radiometric Dating (Age of Rocks)

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9
Q

was the first research vessel specifically designed in the late 1960s for the purpose of drilling into and taking core samples from the deep ocean floor

A

Glomar Challenger

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10
Q

occur along divergent plate boundaries, where new ocean floors are created as the Earth’s tectonic plates spread apart. As the plates separate, molten rock rises to the seafloor, producing enormous volcanic eruptions of basalt.

A

Mid-Ocean Ridge

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11
Q

This theory was proposed by Alfred
Wegener (1912) ; he laid out his
case in his book The Origin of
Continents and Oceans.

A

CONTINENTAL DRIFT THEORY

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12
Q
  • He was a German meteorologist; he
    studied weather.
  • He came up with radical theory that
    suggested that the continents were
    actually once connected and then
    somehow ripped apart to where they
    are today.
  • He proposed a theory that about 200
    million years ago the continents
    were once one large landmass.
    (Wegener could not explain what
    force was driving the motion of the
    continents.);
  • His theory was not accepted by the
    scientific community until 1965 when
    the theory of plate tectonics was
    published.
A

ALFRED WEGENER (1880-1930)

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13
Q

It’s a Greek term that means “Entire
Earth” or all Earth.

A

PANGAEA OR PANGEA

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14
Q

which ran from 541
million to 251.9 million years ago, was a
time of great change on Earth. The era
began with the breakup of one
supercontinent and the formation of another.
Plants became widespread. And the first
vertebrate animals colonized land

A

Paleozoic Era

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15
Q

(252-66 million years ago) means
‘middle life’ and this is the time of the
dinosaurs. This era includes the Triassic,
Jurassic, and Cretaceous Periods.

A

Mesozoic

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16
Q

third of the major eras of
Earth’s history, beginning about 66 million
years ago and extending to the present.

A

The Cenozoic Era

17
Q

is an ancient
freshwater reptile that lived only in
- shallow freshwater only found in
Eastern coast of South America and
Western Coast of Africa

A

Mesosaurus

18
Q
  • means “All Water”
  • A mega ocean that surrounded
    Pangaea.
A

PANTHALASSA

19
Q
  • in the north
A

LAURASIA

20
Q

in the south

A

GONDWANALAND

21
Q

have unique distribution patterns in
some parts of the world.

A

Fossils

22
Q

an English
geologist, proposed the presence of
convection cells in the Earth’s mantle. When
the rocks in the Earth’s interior are heated
by radioactivity, they become less dense,
and they rise toward the surface of the
Earth. When they cool down, they become
denser and sink. The continuous process of
rising and sinking of rocks produces
convection cells or convection currents.
These currents cause the tectonic plates,
which include the crust, to move and drift.

A

Sir Arthur Holmes

23
Q

was a professor of geology
who determined how oceanic mountain
ranges, called mid-ocean ridges, are
fundamental to the tectonic movement that
results in the drift of continents.

A

-Harry Hess

24
Q
  • To establish the age of a rock or a fossil, researchers use some type of clock to determine the date it was formed.
  • determining a chronology or calendar of events in the history of Earth, using to a large degree the evidence of organic evolution in the sedimentary rocks accumulated through geologic time in marine and continental environments.
  • There are a variety of scientific methods that archaeologists use to analyze the age and origins of fossils, remains, or other artifacts.
A

Dating

25
Q

2 methods to determine the age of Fossils

A
  • Relative Dating
  • Absolute Dating
26
Q

methods estimate whether an object is younger or older than other things found at the site. Relative dating does not offer specific dates, it simply allows to determine if one artifact, fossil, or stratigraphic layer is older than another.

A

Relative dating

27
Q

Assuming that soil layers in a deposit accumulate on top of one another, and that the bottom layers will be older than the top layers, stratigraphy allows archaeologists to construct a relative chronological sequence from the oldest (bottom) to youngest (top) layers. Artifacts found in these layers are at least as old as the deposit in which they were found.

A
  1. Stratigraphy
28
Q

A technique that was common in the mid-20th century, seriation looks at changes in certain styles of artifacts present at a site. A chronology is developed based on the assumption that one cultural style (or typology) will slowly replace an earlier style over time.

A
  1. Seriation
29
Q

A technique that analyzes how much of the chemical fluorine has been absorbed by bones from the surrounding soils in order to determine how long the specimen has been underground.

A
  1. Fluorine Dating
30
Q

methods provide more specific origin dates and time ranges, such as an age range in years. How specific these dates can be will depend on what method is used.

A

Absolute dating

31
Q

A technique that determines age of various minerals and glasses based on the trails of damage done by the spontaneous fission of uranium-238, the most abundant isotope of uranium.

A
  1. Fission-track dating
32
Q

Measuring the ratio of argon gas in igneous volcanic rock to estimate how much time has elapsed since the rock cooled and solidified.

A
  1. Potassium-argon dating
33
Q

Magnetic particles in most materials of geological origin, such as rocks and clay, are analyzed to track shifts in the earth’s magnetic fields over time.

A
  1. Archaeomagnetic dating
34
Q

Also known as Radiocarbon dating. Used to date organic substances. Scientists measure the radiocarbon in the fossil to determine its age. Can only date specimens up to about 60,000 years old.

A
  1. Carbon-14 dating (radiocarbon)