Exam 2 Flashcards

(28 cards)

1
Q

Describe the basic units of the coast range geology.

A

“3-layer sandwhich”

  1. Older volcanics in center
  2. Marine sediments in middle
  3. Columbia River Basalt on outside
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2
Q

Describe the structure of the coast range geology.

A

Northward plunging anticline

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3
Q

Describe the 6 major events making up the coastal range’s geologic history.

A
  1. Accretion of island chain onto North American continent
  2. Marine sediments deposited on accreted terrane due to subduction zone jumping westard.
  3. Cascade volcanoes buried eastern edge existing material.
  4. Crustal stretching released CRBs from fissures in east.
  5. “Push” from Juan de Fuca plate causes uplift of Coast Range, folding Coast Range strata into broad arch, with the oldest rocks in center. (anticline)
  6. Missolua floods covered everything beloq 400’ elevation with blanket of silt
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4
Q

List the 4 types of sedimentary rocks, describe process of formation, and give an example of each.

A
  1. Clastic rocks are composed of broken pieces (or clasts) of older weathered and eroded rocks. Classified based on grain size.
    Ex: Sandstone, conglomerate, breccia
  2. Biochemical rocks are formed from organic processes that involve living organisms producing the sediments.
    Ex: limestone, chert.
  3. Chemical rock forms when mineral components in solution become supersaturated and inorganically precipitate.
    Ex: rock salt, gypsum
  4. Organic rocks form from the accumulation and lithification of organic debris, such as leaves, roots, and other plant or animal material.
    Ex: coal, oil shale
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5
Q

List some examples of where you would find sediment (gravel, sand, mud) deposited today.

A
  • Gravel:
    • Landslide
    • Glacier
    • Mountain – River
    • Alluvial fans
    • Pyroclastic flows
  • Sand:
    • Ocean beaches
    • Desert
    • Rivers
    • Pyroclastic flows
  • Mud:
    • Delta
    • Swamp
    • Rivers
    • Lakes
    • Ocean floor
    • Lahar (mudflow mix – diamictite)
    • Pyroclastic flows
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6
Q

Describe what grains can tell you about sedimentary rocks.

A
  • Size indicates energy of flow:
    • Large grains: high energy
    • Small grains: low energy
  • Sorting indicates transport agent:
    • Well sorted: indicates water/wind
    • Poorly sored: indicates ice/ landslide/ mudflows
  • Shape indicates length of transport:
    • Angular: short transport
    • Round: long transport
  • Composition indicates source and maturity:
    • As distance transported increases, mineral variety decreases (weak grains destroyed, resistant grains remain [quartz])
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7
Q

Describe some sedimentary rock structures/formations and their indications.

A
  • Bedding - well defined planes separating stratigraphic rock from layers above and below.
  • Cross bedding - inclined layers formed by wind/river direction
  • Graded bedding - (turbidites) sorted by size; created by underwater landslides (turbidity currents) where coarse grains settle first, fine settle last – so: coarse on bottom, fine on top
  • Mud cracks - formed as muddy sediment dries and contracts
  • Ripple marks - formed by agitation from water or wind
  • Fossils
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8
Q

List the 3 depositional environments and the type of sedimentary rocks they produce.

A
  • Terrestrial: conglomerate, breccia, sandstone, siltstone, shales, coal
  • Coastal: sandstone, shale, limestone
  • Marine: sandstone, siltstone, clay, turbidites, limestone, chert
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9
Q

Describe transgression vs. regression

A
  • Transgression associated with deposits during rising sea level
    (“…oceans transgress onto continents”)
  • Regression associated with deposits during falling sea level
    (“…oceans regress off continents”)
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10
Q

How many known species are there, and how many estimated are there?

A

1-2 million described species

10? million estimate species

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11
Q

Describe body vs. trace vs. chemical fossils

A
  • Body fossils – pieces of organisms
  • Trace fossils – products of an organism’s behavior (ex: foot prints, “chomp marks”)
  • Chemical fossils – chemical traces of past life
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12
Q

Describe some biases of the fossil record.

A
  • Hard parts are favorable
  • Marine setting (low energy environment) is favorable (vs. terrestrial)
  • Anoxic environments (low O2 – so, no decomposition) favorable
  • Cold temperatures favorable
  • Invertebrates (due to structure; shell is entire organism) favorable
    • While vertebrates tend to “fall to pieces” vertebrae by vertebrae
  • Rapid burial circumstances favorable
    • Turbidity currents
    • Ash falls
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13
Q

Describe the difference between a cast vs. mold

A

Organisms buried in sediment can dissolve away leaving a mold.

If the space is filled with sediment, an external cast is made.

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14
Q

Identify this organism, and describe characteristics:

A

Trilobite

  • arthropod, has exoskeleton; results in cast of exoskeleton
  • broken into three parts (across), and three lobes (up/down)
  • very abundant.
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15
Q

Identify this organism and describe some characteristics:

A

Coral

  • Filter feeders
  • Colonial organisms; series of “cups” in which organisms live arranged in various ways
  • Been around since Cambrian; sometimes denser in population, sometimes less
  • Reef corals symbiotic with photosynthetic organisms/ solitary corals can live in deeper waters
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16
Q

Identify this organism and describe some characteristics:

A

Brachiopod

  • Filter feeders; sea water filtered through lophophore
  • Two types: articulate (two shells joined together) or inarticulate (two shells not joined)
  • Shells are symmetrical, but don’t match
17
Q

Identify this organism and describe some characteristics:

A

Bryozoan

  • Moss animals; colonial; grows in mats.
  • Attached to sea floor.
  • Filter feeds.
  • Still alive today.
18
Q

Identify this organism and describe some characteristics:

A

Graptolite

  • Thought to maybe be ancestor to chordates (animals with backbones) (this is debated)
  • Filter feeders
  • Planktonic (float in upper part of water column)
  • Colonial
  • Very small
19
Q

Identify this organism and describe some characteristics:

A

Crinoid

  • “Sea lilies”
  • Stem often breaks into pieces
  • Still alive today
  • Filter feeders living on bottom of seafloor
20
Q

Identify this organism and describe some characteristics:

A

Bivalve

  • Clams
  • Filter feeders
  • Two matching shells; but are asymmetrical
21
Q

Identify this organism:

A

Gastropod

  • Snails
  • Coiled shells; not chambered – one continuous spiral
  • Can be single planes or highly spiraled planes
22
Q

Identify this organism:

A

Ammonite

  • Cephalopods
  • Coiled, chambered shells
  • Control buoyancy or movement by adding water or air to chambers
23
Q

Describe Sepkoski’s Curve

A

Based on marine invertebrates; describes diversity increasing over time “in steps” associated with 3 major faunas:

  1. Cambrian:
  • Trilobites and other arthropods
  • Organisms living on top of mud
  • Little burrowing
  • Little predation
  1. Paleozoic:
  • Brachiopods, crinoids
  • Stalked fauna
  • Burrowing
  • Predators
  1. Modern:
  • Extensive burrowing
  • Very active predation
  • Fewer stalked fauna
24
Q

Describe the structure of an atom:

A
  • Electron cloud (> 99.9% volume)
  • Nucleus (> 99.9% mass)
  • Electrons (e) negative charge
  • Protons (p) positive charge - # determines element
  • Neutrons (n) neutral charge - # determines isotope
    • # Protons vs. # neutrons determine stability
    • Unstable isotopes are radioactive
25
Describe three types of radiation:
* Alpha decay: * Alpha particle emitted α (alpha particle is actually a He nucleus; 2 p + 2 n) * Beta decay: * Emits beta particle β (beta particle is actually a a high energy electron) * Gamma decay: * Gamma rays γ (High energy electromagnetic radiation)
26
Describe parent and daughter elements.
When elements undergo spontaneous decay; parent elements produce daughter element & radioactive rays
27
Describe half life.
* Rate of decay * Statistical (not deterministic) * As time increases, chance of decay increases (but can’t exactly say when it will decay) * So half-life (t1/2) indicates a time at which there is a 50% chance of decay. So, if t \< t1/2 – chance of decay is \< 50% And, if t \> t1/2 – chance of decay is \> 50%
28
Describe how calibrating the time scale occurs.
Geologic time periods are based on sedimentary rocks and fossils. Radiometric dating works best with igneous rocks. So infer ages of sedimentary rocks by dating igneous rocks sandwiching sedimentary layers. (Called: **cross cutting relations** and **bracketing ages**)