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Hydrate Ridge information


Bathymetry of Hydrate Ridge.

Hydrate Ridge is an accretionary thrust clathrate hydrate formation, meaning it has been made of sediment scraped off of subducting oceanic plate. It is approx. 200 m (700 ft) high, and located 100 km (62 mi) offshore of Oregon.[1][2][3] At hydrate formations, methane is trapped in crystallized water structures. Such methane transforms into the gaseous phase and seeps into the ocean at this site, which has been a popular location of study since its discovery in 1986.[4] Hydrate Ridge also supports a methane-driven benthic community.[5]

  1. ^ "The National Methane Hydrates R&D Program". National Energy Technology Laboratory. Retrieved 14 January 2012.
  2. ^ "Hydrate Ridge EXperiment 2004 (HyREX04)". Scripps Institution of Oceanography. 18 March 2011. Retrieved 14 January 2012.
  3. ^ Johnson, J.E.; Goldfinger, C.; Tréhu, A.M.; Bangs, N.L.B.; Torres, M.E.; and Chevallier, J. "North-south variability in the history of deformation and fluid venting across Hydrate Ridge, Cascadia margin." In Tréhu, A.M.; Bohrmann, G.; Torres, M.E.; and Colwell, F.S. (Eds.). Proc. ODP, Sci. Results, 204 (2006): College Station, TX (Ocean Drilling Program), 1–16. doi:10.2973/odp.proc.sr.204.125.2006.
  4. ^ Cite error: The named reference :0 was invoked but never defined (see the help page).
  5. ^ Cite error: The named reference :5 was invoked but never defined (see the help page).

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Hydrate Ridge

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