111-21 - GY 111 Lecture Notes D. Haywick (2008-09) 1 GY 111...

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GY 111 Lecture Notes D. Haywick (2008-09) 1 GY 111 Lecture Note Series Sedimentary Environments 4: Carbonates Lecture Goals A) Shelf Terminology B) Reefs, atolls and oolites C) Evaporites and evaporate basins Reference: Press et al., 2004, Chapter 7; Grotzinger et al., 2007, Chapter 5 pages 108, 120-127; GY 111 Lab manual Chapter 3 A) Shelf Terminology So far in the sedimentology component of GY 111, we have focused on siliciclastic sedimentary environments that were restricted to terrestrial or shoreline areas (e.g., alluvial fans, rivers, deltas, beaches). Today, we start to get our feet wet. Continents are surrounded by relatively shallow water. These are the continental shelves and they are remarkably inconsistent in width. In the Gulf of Mexico near were we live, the shelf is very wide, almost 80 miles in fact. It is also wide along the eastern seaboard of the United States. In contrast, the shelf along the western seaboard of the country (e.g., California, Oregon) is narrow (in some places, only a few miles wide). The reason is that the west coast is a tectonically active region and the Gulf of Mexico/eastern shoreline is not. We call it a passive continental margin which more or less means “boring”, at least as far as volcanoes and earthquakes are concerned. Wide shelves occur along coastlines that are tectonically inactive which are areas where sediment has been being deposited for a long, long, long time. The shelf is officially defined as the region surrounding continents where the water ranges from 10 m 1 to 150 or 200 m in depth. The end of the shelf is marked by a relatively sudden increase in slope at the shelf break (from near 0º on the shelf to 3º along the continental slope ). The deepest part of the ocean (the abyssal plain ) like the shelf is relatively flat, but here is water is incredibly deep (5000 m or more!). Sedimentation on most shelves is restricted to the zone nearest the shoreline. The rest of the shelf may be devoid of any recent sediment. These areas are considered relict because the last time they received sediment was during the height of the last ice age approximately 18,000 years ago. 1 You will recall that the nearshore zone which includes beaches extends outward from the shoreline to the place where the water depth reaches 10 m.
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GY 111 Lecture Notes D. Haywick (2008-09) 2 At this time, sea level was much lower (150m lower) and what is today’s continental shelf was a tree-covered plain. Sea level change is the single most important control of shelf sedimentation. B) Reefs and atolls Siliciclastic shelves are areas where vast quantities of sediment can accumulate. In areas like Mobile where large rivers flow into the sea, sediment that makes it onto the shelf is going to be dominated by siliciclastic grains (remember these are the products of weathering and rivers transport these materials away from the source). In areas where rivers are not as abundant, or the topography is flatter (e.g., the Florida Peninsula), siliciclastic sediment may not
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This note was uploaded on 02/04/2012 for the course GLY 111 taught by Professor Haywick during the Fall '11 term at S. Alabama.

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111-21 - GY 111 Lecture Notes D. Haywick (2008-09) 1 GY 111...

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