Benawang
Dalam geologi, benawang[1] merupakan depresi struktural linier yang memanjang secara lateral pada jarak tertentu. Meskipun tidak setajam palung, benawang dapat berupa cekungan sempit atau retakan geologi. Fitur-fitur ini sering terbentuk di tepi lempeng tektonik .
Terdapat berbagai benawang samudrawi di dasar samudra .
Contoh benawang samudra
- Benawang Benue
- Benawang Cayman [2]
- Benawang Hesperides
- Benawang Raja
- Benawang Mariana
- Benawang Nankai
- Benawang Northumberland
- Benawang Okinawa di Laut Cina Timur
- Benawang Rockall dan lainnya di sepanjang retakan punggungan tengah samudra
- Benawang Salton
- Benawang Shetland Selatan
- Benawang Suakin di Laut Merah
- Benawang Timor [3]
Referensi
- ^ "Benawang - KBBi VI".
- ^ Einsele, Gerhard (2000). Sedimentary Basins: Evolution, Facies, and Sediment Budget (Edisi 2nd). Springer. hlm. 630. ISBN 978-3-540-66193-1.
- ^ "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. Diarsipkan dari asli (PDF) tanggal 20 May 2005.
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