Chapter 1: Earth as a System Flashcards

1
Q

Principles of Actualism

A

fundamental physical & chemical principles observed operating today have operated throughout Earth’s history

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2
Q

Catastrophism

A

global floods caused by supernatural forces formed most of the rocks visible at Earth’s surface.
- Attribute all layers of rocks to series of catastrophes

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3
Q

Principles of Uniformitarianism

A

present is key to the past

  • Somewhat rigid view of Earth’s eternal processes
    § Ex: no events played important geological role - denied by impact of asteroid
    § Ex: all geological changes are gradual - denied by numerous agents which operated with suddenness
    § Ex: all kinds of rocks have never basically changed - denied by new kinds of rocks & organism appear, mammals existed in only 5 percent of planet’s history.
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4
Q

Mineral

A
Naturally occurring
Inorganic 
Solid
Element/ Compound
Particular chemical composition
Characteristic mineral structure/ Crystal lattice
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5
Q

Rock

A

consist of interlocking or bonded grains of matter - typically composed of single minerals

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6
Q

Igneous

A

cooling of molten materials

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7
Q

Sedimentary

A

bonding of loose sediments by compression after burial or precipitation of mineral cement - result of lithification of sediment

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8
Q

Metamorphic

A

alteration of rocks within Earth under conditions of high temp & pressure

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9
Q

Steno’s Law: Principle of Superposition

A

in an undisturbed sequence of data - oldest at bottom & successively higher strata are progressively younger

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10
Q

Steno’s Law: Principle of Original Horizontality

A

all strata are horizontal when they form

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11
Q

Steno’s Law: Principle of Lateral Continuity

A

strata originally are unbroken flat expanses, original continuity can be broken by erosions (ex: when river cuts downward)

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12
Q

Principle of Intrusive Relationship

A

intrusive igneous rock is always younger than the rock that it invades

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13
Q

Principle of Inclusion

A

when fragments of one body of rock are found within a second body, the 2nd is always younger than the 1st.

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14
Q

Unconformity

A

irregular surface between two bodies of rock

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15
Q

Angular Unconformity

A

a group of rocks has been tilted & eroded & younger rocks are deposited on top

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16
Q

Disconformity

A

the irregular surface between the upper & lower rock bodies reveals a past episode of erosion

17
Q

Nonconformity

A

a bedded rocks rest on an eroded surface of crystalline (igneous/ metamorphic) rocks

18
Q

Fossil

A

tangible remains/signs of ancient organism

19
Q

Geological Time Scale

A

Divides Earth’s history into formal units (see side pic)
Divides by the levels in which geologist discover abundant fossils
Eons, Eras, Periods, Epochs
Geological systems
□ Unique group of fossils
□ Nature of rock

20
Q

Core

A

Solid, spherical inner portion

Liquid outer portion - consist mostly of iron

21
Q

Mantle

A

§ Thick envelop around core
§ Complex body of less dense rocky materials
§ Made up most of Earth’s volume

22
Q

Crust

A

still less dense (than mantle & core) rock material

23
Q

Moho - Mohoroviěié discontinuity

A

passage between crust to mantle where waves increase in velocity abruptly

24
Q

Lithosphere

A

crust & upper mantle

25
Q

Asthenosphere

A

“low-velocity zone”, composed of partially molten rock, slush like, solid particles with liquid occupying in between, 10% thickness of mantle

26
Q

Basics of Plate Tectonic

A

the movement of lithospheric plates; driven by convection (process by which material that is heated deep within the asthenosphere rises to displace cooler, less dense material near surface)

27
Q

Type of boundary: Spreading Zones

A

plates move apart, mafic material of relatively low density rise from ultramafic asthenosphere and become new lithosphere, lithosphere slide laterally away
□ Ex: Mid-ocean ridge (Mid-Atlantic)

28
Q

Type of boundary: Subduction Zones

A

plates move back down the asthenosphere along deep-sea trenches

29
Q

Type of boundary: Transform Faults

A

plates slide along each other; faults offset mid-ocean ridges throughout their length

30
Q

Water Cycle

A

see OneNote

31
Q

Darwin’s Theory of Evolution

A

particular kinds of animals & plants gave rise to other kinds
- cyclical but progressional, constantly giving rise to new kinds of organisms

32
Q

Directional changes: Physical

A

cooling of planet’s interior - weakened furnace, plate tectonic weakened, less subduction & spreading zones

33
Q

Directional changes: Chemical

A

shifts of oxygen concentration

34
Q

Ecosystem

A

an environment together with the group of organisms that lives within it.
- Environmental change influenced ecosystems. Study of ancient ecosystems let geologists know how to confront future environmental changes.