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Conglomerate (geology): Map

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Conglomerate, Submarine Landslide located at Point Reyes, Marin County California.


A conglomerate ( ) is a rock consisting of individual clasts within a finer-grained matrix that have become cemented together. Conglomerates are sedimentary rocks consisting of rounded fragments and are thus differentiated from breccias, which consist of angular clasts."Conglomerate Rocks." Conglomerate Rocks on Rock Hound. Rock Hounds. Retrieved on July 29, 2007. Both conglomerates and breccias are characterized by clasts larger than sand (>2 mm).

Classification

In addition to the factors described in this section, conglomerates are classified in terms of both their rounding and sorting.

Texture

Paraconglomerates consist of a matrix-supported rock that contains at least 15% sand-sized or smaller grains (<2&NBSP;MM), the="" rest="" being="" larger="" grains="" of="" varying="" sizes."Paraconglomerates."</2&NBSP;MM),> <2&NBSP;MM), the="" rest="" being="" larger="" grains="" of="" varying="" sizes.Paraconglomerates on Biodatabase.</2&NBSP;MM),> <2&NBSP;MM), the="" rest="" being="" larger="" grains="" of="" varying="" sizes.Biodatabase.</2&NBSP;MM),> <2&NBSP;MM), the="" rest="" being="" larger="" grains="" of="" varying="" sizes.Retrieved on July 29, 2007.

Orthoconglomerates consist of a clast-supported rock with less than 15% matrix of sand and finer particles."Orthoconglomerates." Orthoconglomerates on Biodatabase. Biodatabase. Retrieved on July 29, 2007.

Metamorphic alteration transforms conglomerate into metaconglomerate.

Clast composition

Conglomerates are classified for the lithologies of the clasts
  • Monomict - clasts with only a single lithology
  • Oligomict - clasts of only a few different lithologies
  • Polymict - clasts of many different lithologies
  • Intraformational - clasts derived from the same formation in which they are found
  • Extraformational - clasts derived older rocks than the formation in which they are found


Clast size

Conglomerates are also classified by the dominant clast size.

  • Granule conglomerate 2–4 mm
  • Pebble conglomerate 4–64 mm
  • Cobble conglomerate 64–256 mm
  • Boulder conglomerate >256 mm


Sedimentary environments

Conglomerates are deposited in a variety of sedimentary environments.

Deepwater marine

In turbidites, the basal part of a bed is typically coarse-grained and sometimes conglomeratic. In this setting, conglomerates are normally very well sorted, well-rounded and often with a strong A-axis type imbrication of the clasts.

Shallow marine

Conglomerates are normally present at the base of sequences laid down during marine trangression above an unconformity, and are known as basal conglomerates. They represent the position of the shoreline at a particular time and will be diachronous.

Fluvial

Conglomerates deposited in fluvial environments are typically well-rounded and well-sorted. Clasts of this size are carried as bedload and only at times of high flow-rate. The maximum clast size decreases as the clasts are transported further due to attrition, so conglomerates are more characteristic of immature river systems. In the sediments deposited by mature rivers, conglomerates are generally confined to the basal part of a channel fill where they are known as pebble lags. Conglomerates deposited in a fluvial environment often have an AB-plane type imbrication.

Alluvial

Alluvial deposits are formed in areas of high relief and are typically coarse-grained. At mountain fronts individual alluvial fans merge together to form braidplains and these two environments are associated with the thickest deposits of conglomerates. The bulk of conglomerates deposited in this setting are clast-supported with a strong AB-plane imbrication. Some matrix-supported conglomerates are present, a result of debris-flow deposition on some alluvial fans.

Glacial

Glaciers carry a lot of coarse-grained material and many glacial deposits are conglomeratic. Tillite, the sediments deposited directly by a glacier, are typically poorly-sorted, matrix-supported conglomerates. The matrix is generally fine-grained, consisting of finely milled rock fragments. Waterlain deposits associated with glaciers are often conglomeratic, forming structures such as eskers.

Examples

A spectacular example of conglomerate can be seen at Montserratmarker, near Barcelonamarker. Here erosion has created vertical channels giving the characteristic jagged shapes for which the mountain is named (Montserrat literally means "jagged mountain"). The rock is strong enough to be used as a building material - see Montserrat abbey front at full resolution for detail of the rock structure.

Another spectacular example of conglomerate, the Crestone Conglomerate may be viewed in and near the town of Crestonemarker, at the foot of the Sangre de Cristo Range in Coloradomarker's San Luis Valley. The Crestone Conglomerate is a metamorphic rock stratum and consists of tiny to quite large rocks that appear to have been tumbled in an ancient river. Some of the rocks have hues of red and green.

Conglomerate may also be seen in the domed hills of Kata Tjutamarker, in Australia's Northern Territorymarker.

Pottsville conglomerate
In the nineteenth century a thick layer of Pottsville conglomerate was recognized to underlie anthracite coal measures in Pennsylvania.

Fanglomerate

Fanglomerate
When a series of conglomerates accumulates into an alluvial fan, in rapidly eroding (e.g. desert) environments, the resulting rock unit is often called a fanglomerate. These form the basis of a number of large oil fields, e.g. the Tiffany and Brae fields in the North Seamarker. These fanglomerates were actually deposited into a deep marine environment but against a rapidly moving fault line, which supplied an intermittent stream of debris into the conglomerate pile. The sediment fans are several kilometers deep at the fault line and the sedimentation moved focus repeatedly, as different sectors of the fault moved.

See also



References

  1. Nichols, G.P. 2009. Sedimentology and stratigraphy, 2nd edition, WileyBlackwell 432pp.
  2. Walker, R.G. 1979. Facies Models. Reprinted with revisions from a series of papers in Geoscience Canada, 1976-1979, Geological Association of Canada, 211pp.
  3. Seibold, E. & Berger, W.H. 1996. The Sea Floor: an introduction to Marine Geology, Springer, 356pp.
  4. Tucker, M.E. 2001. Sedimentary petrology, 3rd edition, WileyBlackwell, 272pp.


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