Lecture 8

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Lecture 8 All the rivers run to the sea, yet the sea is not full: unto the place from whence the rivers come, thither they return again. - Ecclesiastes 1:7 Sedimentary Rocks Webpage for course (dayt ime) Webpage for course (nigh ttime)

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All the rivers run to the sea, yet the sea is not full: unto the place from whence the rivers come, thither they return again. - Ecclesiastes 1:7 Sedimentary Rocks. Lecture 8. Webpage for course (daytime). Webpage for course (nighttime). - PowerPoint PPT Presentation

Transcript of Lecture 8

Page 1: Lecture 8

Lecture 8

All the rivers run to the sea, yet the sea is not full: unto the place from whence the rivers come, thither they return again.

- Ecclesiastes 1:7

Sedimentary Rocks

Webpage for course (daytime)

Webpage for course (nighttime)

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Three types of rocks:

- Igneous-Sedimentary- Metamorphic

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Sedimentary rocks are important because

Form and are common at earth’s surfacePreserve the history of Life (contain fossils)

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Sedimentary rocks are important because

Form and are common at earth’s surfacePreserve the history of Life (contain fossils)Show past environments, climatesProvide a geologic record of past historyMajor sources of energy – oil, gas, coal

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General History of a Sedimentary Rock

WEATHERINGTRANSPORTATIONDECOMPOSITIONDEPOSITIONLITHIFICATION

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Mechanisms of Transportation and Deposition

Water - streams, rivers, etc., freshwater and marine

Wind Gravity – downslope movementIce – glaciers

Some sedimentary rocks form of atoms dissolved in water and precipitated elsewhere

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Classification of sedimentary rocks

Clastic (Detrital in your book)

Nonclastic

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Nonclastic

Example, coal

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Nonclastic

Another example, rock salt

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Clastic

Classification depends on grain size

Size (mm) particle name >256 64-256 4-64 2-4 .0625-2 .0039-.0625 <0.0039

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Clastic

Classification depends on grain size

Size (mm) particle name rock name >256 boulder 64-256 cobble 4-64 pebble 2-4 granule .0625-2 sand .0039-.0625 silt <0.0039 clay

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Clastic

Classification depends on grain size

Size (mm) particle name rock name >256 boulder 64-256 cobble 4-64 pebble 2-4 granule .0625-2 sand sandstone .0039-.0625 silt <0.0039 clay

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Clastic

Classification depends on grain size

Size (mm) particle name rock name >256 boulder 64-256 cobble conglomerate 4-64 pebble or breccia 2-4 granule .0625-2 sand sandstone .0039-.0625 silt siltstone <0.0039 clay shale

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Why the distinction conglomerate and breccia?

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Conglomerate means slow, breccia means sudden

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Nonclastic

Chemical Biogenic

CoalCoquinaChalkDiatomite

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Diatoms

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Nonclastic

Chemical

Rock SaltChertLimestoneDolomite

Biogenic

CoalCoquinaChalkDiatomite

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Coal as Energy