Temporary Disabled. :) please Go back Trough (geology) - Wikipedia www.fgks.org » Address: [go: up one dir, main page] Include Form Remove Scripts Accept Cookies Show Images Show Referer Rotate13 Base64 Strip Meta Strip Title Session Cookies Home Random Nearby Log in Settings Donate About Wikipedia Disclaimers Search Trough (geology) Article Talk Language Watch Edit (Redirected from Geologic trough) This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed.Find sources: "Trough" geology – news · newspapers · books · scholar · JSTOR (June 2023) (Learn how and when to remove this message) For troughs created by glaciation, see Glacial trough. In geology, a trough is a linear structural depression that extends laterally over a distance. Although it is less steep than a trench, a trough can be a narrow basin or a geologic rift. These features often form at the rim of tectonic plates. Satellite image of the Cayman Trough Bathymetric features of the Rockall Trough northwest of Scotland and Ireland There are various oceanic troughs on the ocean floors. Examples of oceanic troughs edit Benue Trough Cayman Trough[1] Hesperides Trough Kings Trough Mariana Trough Nankai Trough Northumberland Trough Okinawa Trough in the East China Sea Rockall Trough and others along the rift of the mid-oceanic ridge Salton Trough South Shetland Trough Suakin Trough[2] in the Red Sea Timor Trough[3] See also edit Walker Lane Oceanic basin References edit ^ Einsele, Gerhard (2000). Sedimentary Basins: Evolution, Facies, and Sediment Budget (2nd ed.). Springer. p. 630. ISBN 978-3-540-66193-1. ^ Dinwiddie, Robert et al. (2008) Ocean: The World's Last Wilderness Revealed, London, Dorling Kindersley, page 452. ^ "Chapter II (Geology of Timor-Leste)". Atlas of mineral resources of the ESCAP region Volume 17 Geology and Mineral Resources of Timor-Leste (PDF). United Nations Economic and Social Commission for Asia and the Pacific. 24 December 2003. Archived from the original (PDF) on 20 May 2005. This geomorphology article is a stub. You can help Wikipedia by expanding it.vte
In geology, a trough is a linear structural depression that extends laterally over a distance. Although it is less steep than a trench, a trough can be a narrow basin or a geologic rift. These features often form at the rim of tectonic plates.
There are various oceanic troughs on the ocean floors.
This geomorphology article is a stub. You can help Wikipedia by expanding it.