ESCI Exam 1 Flashcards

(46 cards)

1
Q

human population and the environment,resources + pollution

A

resources: more people require more resources like food, energy, and water
pollution: more people means more waste including plastic, chemicals, and greenhouse gasses

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2
Q

challenges in achieving comfortable living standards

A
  1. resource scarcity, competition
  2. environmental degradation, soil erosion
  3. social and economic strain
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3
Q

present world population

A

8 billion

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4
Q

population growth rates compared

A

recent population growth rates are higher due to the industrial revolution and advancements in technology

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5
Q

doubling time

A

the amount of time it takes for a value to double itself at a consistent rate of growth. Divide 70/annual growth rate.
advancements in technology and medicine

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6
Q

what regions have the fastest and slowest population growth

A

Highest: Africa and Asia
Slowest: Europe and North America

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7
Q

Ion

A

an atom that is positively or negatively charged

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8
Q

Isotope

A

elements with different number of neutrons

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9
Q

Compound

A

a substance formed when two or more chemical elements are bonded

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10
Q

mineral

A

naturally occurring inorganic solid with chemical composition and crystalline structure

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11
Q

rock

A

any naturally occurring solid mass or aggregate of minerals or mineraloid matter

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12
Q

What two properties define a particular mineral

A

chemical composition and crystalline structure

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13
Q

what is an igneous rock? Volcanic vs. plutonic

A

a rock that forms from the solidification of molten rock material, smaller minerals equal quick cooling

volcanic/intrinsic: formed from lava that erupted onto the Earth’s surface,

Plutonic/extrinsic: formed from magma that cools and solidifies beneath the surface, larger minerals equal longer cooling time

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14
Q

how do igneous rocks form

A

melting crystallization, complete melt

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15
Q

what mineral group is most common in igneous rocks

A

silicates are made up of silicon and oxygen, quartz, feldspar, mica, and olivine

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16
Q

porphyritic texture, how it’s formed

A

large, well formed crystals embedded in finer grain matrix, formed when magma undergoes 2 stages of cooling first to form the large crystals and then to form the finer grains

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17
Q

principles of sedimentary rock

A
  1. clastic: formed by the lithification of
    mechanically weathered pieces of rocks and minerals: conglomerate, sandstone, shale
  2. chemical and biochemical: minerals precipitate from the
    water and can form thick
    deposits limestone, halite
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18
Q

common physical weathering processes

A

Frost wedging: water freezes in cracks
root wedging: plant roots grow into cracks
abrasion: rubbing wears down the surface
physical weather
unloading: change of pressure

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19
Q

effects weathering has on chemical weathering

A

exposure of fresh surfaces: may contain minerals more susceptible to weathering
increased surface area: more area for chemical reactions to occur
transportation: transport rocks into new environments where they may be exposed to acid

chemical reactions that break down into solutes and byproducts

20
Q

Principle of Superposition

A

younger rocks on top, older rocks on the bottom

21
Q

sources of heat or pressure in metamorphism

A

heat from magma, heat from earths interior, pressure from overlaying rock, tectonic forces

22
Q

contact metamorphism vs. regional metamorphism

A

contact: a type of metamorphism where rock minerals and texture are changed, by heat, due to contact with magma, elevated temperature no pressure

regional: large scale stressing and heating of a rock
by deep burial or continental plates moving and colliding

23
Q

foliation, how it’s formed

A

when a rock is subjected to directed stress, its minerals form elongated/platy crystals and line up
parallel to each other

24
Q

causes of strain in rock, plastic vs. brittle materials

A

strain is caused by stress which leads to deformation, compression, separation, slide past each other

plastic: undergo deformation without fracturing
brittle: fracture under stress when elastic limit is exceeded

25
plate tectonic, continental drift and seafloor spreading relationship
large scale motion of lithosphere and plate tectonics continental drift: continents were once joined seafloor spreading: crust is formed at mid ocean ridges as tectonic plates pull apart they are both driven by the motion of the tectonic plates
26
paleomagnetic evidence
magnetic reversal: magnetic poles have not always been in the same location dating mechanism for movement of continents and formation of new oceanic crust
27
occurence of plate tectonics
1. distribution of earthquakes and volcanos 2. fossil evidence 3. hot spots 4. continental drift
28
subduction zone formation, what process happens at this plate boundary
forms at convergent plate where two plates collide and one is forced beneath the other, dense plate goes underneath earthquakes, volcanic activity
29
how continent convergence happens and what happens
when two plates collide mountain building, earthquakes, crustal thickening, no subduction continent convergence leads to the formation of some of the worlds largest mountain ranges and a key process in shaping the Earth's surface Himalayas and Alpes
30
hot spots, determining rates and direction of plate movement
areas of volcanic activity that are thought to be caused hot spots a chain of volcanic islands are formed as plates move over hot spot
31
shield volcanoes, why not hazardous
shallow and dome shape, gradual accumulation of lava layers that form the shield shape, they have gentle eruptions which make them not hazardous
32
eruptive style of St. Helens compared to Hawaii
Stratovolcano- Mt. St. Helens has more explosive eruptions with ash clouds, and pyroclastic flows
33
pyroclasts
fragments of volcanic rock and glass during explosive eruptions
34
comparing active, dormant, and extinct volcanos, limitations of classification scheme
active: currently erupting, have recently, or are expected to erupt in the near future dormant: currently inactive but have the potential to erupt again extinct: not expected to erupt again, may have eroded and may no longer have a recognizable structure classification scheme only works for human history "recent history" is short geologically
35
volcanic explosivity index
a scale used to measure the explosiveness of volcanic eruptions based on various factors 0-8
36
precede volcanic eruptions
1. seismic activity: small earthquakes or tremors 2. gas emissions: changes in gas emissions can indicate increased activity
37
Yellowstone supervolcano
origins associated with a hot spot supervolcano: the scale of its past eruptions capable of producing VEI 8
38
fault creep, damaging earthquakes
slow movement along fault which relieves pressure and stress which calms bigger earthquake events. if it gets stuck, it can build stress which can lead to an earthquake
39
earthquakes and elasticity
elastic behavior allows them to store and release stress, rock can change shape and return to their original shape when stress is removed once elastic limit is exceeded rocks deform plastically causing an earthquake
40
strike slip vs dip slip faults
strike slip: the movement of rock occurs horizontally along the fault plane, moving laterally dip slip: the movement of rocks occur vertically along the fault plane normal and reverse
41
magnitude vs intensity
magnitude: the size of an earthquake and the amount of energy released, determined using seismographs, measured using the richter scale intensity: the effects of an earthquake, based on observations of shaking and damage, uses the Modified Mervalli Intensity scale (MMI) from I-XII
42
granite into sedimentary
igneous granite weathering and lithifying turning into a sedimentary rock
43
Felsic
light colored minerals, cooler magma, intrusive, granite
44
Intermediate
light and dark minerals, medium temp, intrusive, diorite
45
Mafic
hotter magma, dark color, extrusive, basalt
46
rock cycle in terms of plate tectonics, creation of new igneous, metamorphic, and sedimentary rocks.
igneous: as lava reaches earth's surface, it cools and becomes an extrusive igneous rock metamorphic: the areas around the magma chambers create metamorphic rock from contact metamorphism sedimentary: as sediment settles and hardens, sedimentary rocks form