cayman trough wikipedia - EAS
- Xem thêmXem tất cả trên Wikipediahttps://en.wikipedia.org/wiki/Cayman_Trough
The Cayman Trough (also known as the Cayman Trench, Bartlett Deep and Bartlett Trough) is a complex transform fault zone pull-apart basin which contains a small spreading ridge, the Mid-Cayman Rise, on the floor of the western Caribbean Sea between Jamaica and the Cayman Islands. It is
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Xem thêm• Goreau, P. D. E. 1983 Tectonic Evolution of the North Central Caribbean Plate Margin. Woods Hole Oceanographic Institution, MA.; Massachusetts Inst. of Tech., Cambridge. Sponsor: National Science Foundation, Washington, DC. Sep 1983. 248p. Report: WHOI
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- https://en.wikipedia.org/wiki/Talk:Cayman_Trough
As for a google search: "Cayman trough" gets 9920 hits whereas "Cayman trench" gets 14,800 (note the " " were in the search to get a direct match). That is a bit more, but look at the quality of the hits: trough gets more scientific hits versus trench getting more general hits. Interesting to note that the Wikipedia article is the first link ...
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- https://en.wikipedia.org/wiki/Cayman_Islands
The islands are in the western Caribbean Sea and are the peaks of an undersea mountain range called the Cayman Ridge (or Cayman Rise). This ridge flanks the Cayman Trough, 6,000 m (20,000 ft) deep which lies 6 km (3.7 mi) to the south. The islands lie in the northwest of the Caribbean Sea, east of Quintana Roo, Mexico and Yucatán State, Mexico, northeast of Costa Rica, north of Panama, …
Wikipedia · Nội dung trong CC-BY-SA giấy phép - https://en.wikipedia.org/wiki/2020_Caribbean_earthquake
Tectonic setting. The eastern part of the Cayman Trough forms part of the Gonâve Microplate, which lies between the North American Plate and the Caribbean Plate.It is bounded to both north and south by large transform faults that together accommodate the relative displacement of the two major plates. To the north the boundary is the western part of the Septentrional-Oriente …
- Local time: 14:10:25
- Local date: 28 January 2020
- UTC time: 2020-01-28 19:10:24
Trogolo Cayman - Cayman Trough - abcdef.wiki
https://it.abcdef.wiki/wiki/Cayman_TroughLa Cayman Trough (noto anche come Cayman Trench, Bartlett profonda e Bartlett Trogolo) è un complesso trasformare guasto zona bacino di pull-apart che contiene una piccola cresta diffusione, l' aumento Mid-Cayman, sul pavimento del western Caraibi tra Giamaica e le Isole Cayman. È il punto più profondo del Mar dei Caraibi e fa parte del confine tettonico tra la …
Fosa de las Caimán - Wikipedia, la enciclopedia libre
https://es.wikipedia.org/wiki/Fosa_de_las_CaimánTen Brink, Uri S., et al., 2001, Asymmetric seafloor spreading, crustal thickness variations and transitional crust in Cayman trough from gravity, GSA Meeting Abstract; Roberts, H. H. 1994 Reefs and lagoons of Grand Cayman Monographiae biologicae (Brunt, MA; Davies, JE eds). Kluwer Academic Publishers, Boston, Ma The Hague. ISBN 0-7923-2462-5
- https://en.wikipedia.org/wiki/Beebe_Hydrothermal_Vent_Field
The Beebe Hydrothermal Vent Field (also known as the Piccard Vent Field) is located just south of Grand Cayman in the Caribbean, on the north side of the Mid-Cayman Spreading Centre in the Cayman Trough. Approximately 24 kilometres (15 mi) south of Beebe is the Von Damm Vent Field.. At nearly 5,000 metres (16,000 ft) below sea level, Beebe is the world's deepest known …
Wikizero - Cayman Trough
https://wikizero.com/www//Cayman_TrenchCayman Trench | Science and the Sea
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