Chevron (land form)

From Wikipedia, the free encyclopedia
Jump to: navigation, search
This article is about deposits of sediment across the earth's surface. For folds in rock layers, see Chevron (geology).

A chevron is a wedge-shaped sediment deposit observed on coastlines and continental interiors around the world. The term chevron was originally used independently by Maxwell and Haynes[1] and Hearty and others[2] for large, v-shaped, sub-linear to parabolic landforms in southwestern Egypt and on islands in the eastern, windward Bahamas. The Egyptian “chevrons” are active, wind-generated dunes, but the “chevrons” in the Bahamas are inactive and have been variously interpreted.[3] The most common interpretation of large, chevron-shaped bed forms is that they are a form of parabolic dune, and that most examples are generated by wind action.

In an alternative view, the Holocene Impact Research Group hypothesizes that the formations could be caused by tsunamis from meteorite impacts or submarine slides which lift sediment up and carry it hundreds of miles until depositing it on coastlines.[4] Part of the evidence they cite for this hypothesis is that the sediments contain tiny marine fossils; however, such fossils can be moved by the wind, just like sand. The impact idea is controversial not only because chevrons are similar to wind-blown landforms found far from the ocean, but also because it is unlikely that there have been enough large impacts and landslides to explain the observed chevrons. Moreover, some computer models and sediment-transport analysis do not support this theory. For example, the orientation of chevrons along the southern coast of Madagascar do not line up with what these models of mega-tsunamis have simulated.[5] Additional evidence against the mega-tsunami hypothesis is that the force of the water would not produce such regular bed forms.[3]

Many chevrons can be found in Australia,[6] but others are concentrated around the coastlines of the world. For instance there are chevrons in Hither Hills State Park on Long Island and in Madagascar (such as the Fenambosy Chevron), as well as in interior sites of the United States such as the Palouse region of eastern Washington State, the Great Sand Dunes National Park and Preserve, and White Sands National Monument.

Notes[edit]

  1. ^ Maxwell, T.A. and Haynes, C.V., Jr., 1989. Large-scale, low-amplitude bedforms (chevrons) in the Selima Sand Sheet, Egypt: Science v. 243, p. 1179-1182.
  2. ^ Hearty, Paul J.; A. Conrad Neumann; Darrell S. Kaufman (1998). "Chevron Ridges and Runup Deposits in the Bahamas from Storms Late in Oxygen-Isotope Substage 5e". Quaternary Research 50: 309–322. Retrieved 15 February 2013. 
  3. ^ a b Bourgeois, Joanne; Robert Weiss (2009). "'Chevrons' are not mega-tsunami deposits—A sedimentologic assessment". Geology 37 (5): 403–406. doi:10.1130/G25246A.1. Retrieved 15 February 2013. 
  4. ^ Gusiakov, V. Abbott, D.H., Bryant, E.A., Masse, W.B., and Breger, D., 2010. Mega tsunami of the world oceans: Chevron dune formation, micro-ejecta, and rapid climate change as the evidence of recent oceanic bolide impacts: T. Beer (ed.), Geophysical Hazards, p. 197-227; Springer Publ.
  5. ^ "Contrary to recent hypothesis, 'chevrons' are not evidence of megatsunamis". Phys.Org. 29 April 2009. Retrieved 15 February 2013. 
  6. ^ Scheffers, Anja; Kelletat, Dieter (2003). "Chevron-shaped Accumulations Along the Coastlines of Australia As Potential Tsunami Evidences?". Science of Tsunami Hazards 21 (3): 174–188. Retrieved 15 February 2013. 

References[edit]