Chapter 5 (part 2) Flashcards

1
Q

The characteristics of sediment deposited in an area depend on:

A
  • Tectonic setting
  • Physical, chemical, and biological processes in the depositional environment
  • Method of sediment transport
  • Rocks in the source area from which the sediment is derived
  • Climate <em>(and its effect on weathering)</em>
  • Post-depositional processes of lithification <em>(cementation, compaction)</em>
  • Time
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2
Q

In regard to Tectonics, an area may be in one of these 4 states:

A
  • Tectonically Stable <em>(e.g., midwestern U.S.)</em>
  • Subsiding <em>(or sinking e.g., New Orleans or Mexico City)</em>
  • Rising Gently <em>(e.g., New England and parts of Canada after glacial retreat)</em>
  • Rising Actively <em>(to produce mountains and plateaus e.g., parts of Oregon in the Cascade mountains)</em>
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3
Q

Sediments and sedimentary rocks may be ____ or ____ In Origin.

A

• Extrabasinal
<em>(formed from the weathering of pre-existing rocks outside the basin, and transported to the environment of deposition.)</em>
• Intrabasinal
<em>(formed inside the basin; includes chemical precipitates, most carbonate rocks, and coal.)</em>

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4
Q

What are three broad categories of depositional environments:

A
  • Marine
  • Transitional
  • Continental
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5
Q

The 4 components of Marine Depositional Environments are:

A
  • Continental Shelf
  • Continental Slope
  • Continental Rise
  • Abyssal Plain
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6
Q

The types of Transitional Depositional Environments at or near the transition between the land and the sea are:

A
  • Deltas
  • Beaches
  • Barrier Islands
  • Lagoons
  • Tidal Flats
  • Estuaries
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7
Q

The 5 types of Continental Environments are:

A
  • Fluvial
  • Alluvial Fans
  • Lacustrine
  • Glacial
  • Eolian
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8
Q

The three “textural components” to most clastic sedimentary rocks are:

A
  • Clasts
  • Matrix
  • Cement
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9
Q

What are 3 sedimentary structures that form after deposition?

A
  • Footprints
  • Worm Trails
  • Mudcracks
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10
Q

The 4 major types of sandstone are:

A

Quartz
Arkose
Graywacke
Lithic

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11
Q

The characteristics of most marine carbonate environments include:

A
  • Warm Water
  • Shallow Water
  • Tropical Climate
  • Clear Water
  • Sunlight
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12
Q

The 3 causes of Transgressions are:

A
  • Melting of Polar Ice Caps
  • Displacement of Ocean Water by Undersea Volcanism
  • Localized Sinking or Subsidence of the Land in Coastal Areas.
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13
Q

The 3 causes of Regressions are:

A

Buildup of ice in the polar caps
Formation of Glaciers
Localized uplift of land in coastal areas

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14
Q

Walther’s Principle explains that:

A

Sedimentary Environments that started out side-by-side will end up overlapping one anotherover time due to sea level change. The Vertical Sequence of Facies mirrors the Original Lateral Distribution of Sedimentary Environments.

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15
Q

The two basic types of contacts between rock units are:

A
  • Conformable
  • Unconformable
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16
Q

Conformable contacts between beds of sedimentary rocks may be either:

A

Abrupt or Gradational

17
Q

Unconformable contacts (or unconformities) are surfaces which represent a gap in the geologic record, because of either:

A

Erosion or Nondeposition

18
Q

The 3 types of unconformities are:

A
  • Angular Unconformity
  • Nonconformity
  • Disconformity
19
Q

The various ways in which the distribution of rocks can be depicted are:

A
  • Geologic Columns
  • Stratigraphic Cross-Sections
  • Structural Cross-Sections
  • Geologic Maps
  • Paleogeographic Maps
  • Isopach Maps
  • Lithofacies Maps