Principles Of Geology at Bicol University | Flashcards & Summaries

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Lernmaterialien für Principles of Geology an der Bicol University

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The assumption that the same natural laws and processes that operate in our present-day scientific observations have always operated in the universe in the past and apply everywhere in the universe. (James Hutton)

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Uniformitarianism

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The main stream, which functions as a channelway  through which water and sediment move from the collecting area toward the ocean. It may also collect additional water and sediment. 

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Transportation System

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It lies between Upper Mantle and Lower Mantle

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Repiti Discontinuity

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The differential, or partial, melting of rocks. Each mineral in a rock has its own melting temperature, which is decreased to varying degrees by its close association with other minerals.

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Anatexis

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One of a class of bodies that are theorized to have coalesced to form Earth and other planets after condensing from concentrations of diffuse matter early in the history of the solar system. 

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Planetesimal 

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Any chemical, physical, or biological process that affects a sedimentary earth material after initial deposition, and during or after lithification, exclusive of weathering and metamorphism.


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Diagenesis

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It lies between the Upper and Lower Core

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Lehman Discontinuity

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Are more coarse-grained, represented mostly by sands and breccias, where alluvial sands resulted from the reworking of aeolian sands. 

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Alluvial Deposits

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Is a short interruption in sedimentation with little or no erosion. 

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Diastem 

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A break or interruption in the continuity of the geologic record, such as the absence in a stratigraphic sequence of rocks that would normally be present but either was never deposited or was eroded before deposition of the overlying beds. 

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Hiatus

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It is a shallow body of water separated from a larger body of water by a narrow landform, such as reefs, barrier islands, barrier peninsulas, isthmuses.

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Lagoon 

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It lies between the Mantle and the Core

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Gutenberg Discontinuity

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Q:

The assumption that the same natural laws and processes that operate in our present-day scientific observations have always operated in the universe in the past and apply everywhere in the universe. (James Hutton)

A:

Uniformitarianism

Q:

The main stream, which functions as a channelway  through which water and sediment move from the collecting area toward the ocean. It may also collect additional water and sediment. 

A:

Transportation System

Q:

It lies between Upper Mantle and Lower Mantle

A:

Repiti Discontinuity

Q:

The differential, or partial, melting of rocks. Each mineral in a rock has its own melting temperature, which is decreased to varying degrees by its close association with other minerals.

A:

Anatexis

Q:

One of a class of bodies that are theorized to have coalesced to form Earth and other planets after condensing from concentrations of diffuse matter early in the history of the solar system. 

A:

Planetesimal 

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Q:

Any chemical, physical, or biological process that affects a sedimentary earth material after initial deposition, and during or after lithification, exclusive of weathering and metamorphism.


A:

Diagenesis

Q:

It lies between the Upper and Lower Core

A:

Lehman Discontinuity

Q:

Are more coarse-grained, represented mostly by sands and breccias, where alluvial sands resulted from the reworking of aeolian sands. 

A:

Alluvial Deposits

Q:

Is a short interruption in sedimentation with little or no erosion. 

A:

Diastem 

Q:

A break or interruption in the continuity of the geologic record, such as the absence in a stratigraphic sequence of rocks that would normally be present but either was never deposited or was eroded before deposition of the overlying beds. 

A:

Hiatus

Q:

It is a shallow body of water separated from a larger body of water by a narrow landform, such as reefs, barrier islands, barrier peninsulas, isthmuses.

A:

Lagoon 

Q:

It lies between the Mantle and the Core

A:

Gutenberg Discontinuity

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