To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Gray's Reef National Marine Sanctuary

From Wikipedia, the free encyclopedia

Gray's Reef National Marine Sanctuary
IUCN category IV (habitat/species management area)
Sponges in Gray's Reef NMS
LocationGeorgia, USA
Nearest citySavannah, GA
Coordinates31°25′N 80°55′W / 31.417°N 80.917°W / 31.417; -80.917
Area57 km2 (22 sq mi)
EstablishedJanuary 16, 1981[1]
Governing bodyNational Oceanic and Atmospheric Administration
Map

Gray's Reef National Marine Sanctuary is one of the largest near shore live-bottom reefs in the southeastern United States. The sanctuary, designated in January 1981, is located 19 miles (31 km) off Sapelo Island, Georgia, and is one of 14 marine sanctuaries and monuments that make up the U.S. National Marine Sanctuary System.

Within the 22-square-mile (57 km2) sanctuary, there are both rocky ledges and sandy flat places. The reef's rocky sandstone outcrops, submerged beneath 60 to 70 feet (18 to 21 m) of water, can be as tall as 2 to 3 m and are highly complex.[2] These nooks and crannies provide plenty of places for invertebrates to latch on to and for fish to hide in. Together these animals form a dense tapestry of living creatures that in places completely hides the rock. That gives the habitat of Gray's Reef its common name — a "live bottom".

Researchers from NOAA and the University of Georgia have used the site to study invertebrate and vertebrate paleontology as well as the effects of erosion.[2]

YouTube Encyclopedic

  • 1/1
    Views:
    2 079
  • Diving at Gray's Reef National Marine Sanctuary

Transcription

Human occupation

Although Gray's Reef is more than 19 miles (31 km) beyond today's shoreline, and 60 to 70 feet (18 to 21 m) below the Atlantic Ocean, it was once dry land and part of the mainland as recently as 8,000 years ago.[3] Human occupation of this area dates back at least 13,250 years, and coincides with one of the most dramatic periods of climate change in recent earth history, toward the end of the Ice Age, in the Late Pleistocene epoch. Sea levels were more than 200 feet lower than present levels, and the Atlantic Ocean and Gulf of Mexico shorelines were 100 or more miles seaward of their present locations.[4] A 2003 research project undertaken by University of Georgia researchers Ervan G. Garrison, Sherri L. Littman, and Megan Mitchell, looked at and reported on the Gray's Reef fossils and artifacts, including artifacts from a period of occupation by Clovis culture and Paleoindian hunters dating back more than 10,000 years.[citation needed]

References

  1. ^ 42 FR 7942. Retrieved from https://www.govinfo.gov/content/pkg/FR-1981-01-26/pdf/FR-1981-01-26.pdf
  2. ^ a b Noakes, SE; Garrison, EG; McFall, GB (2009). "Underwater Paleontology: Recovery of a Prehistoric Whale Mandible Offshore Georgia". In: Pollock NW, ed. Diving for Science 2009. Proceedings of the American Academy of Underwater Sciences 28th Symposium. Dauphin Island, AL. Archived from the original on September 6, 2013. Retrieved 2013-05-07.{{cite journal}}: CS1 maint: unfit URL (link)
  3. ^ Thomas Thurman. "The arrival of humans in Georgia". GeorgiaFossils.com. Retrieved November 9, 2018.
  4. ^ David G. Anderson, University of Tennessee, Knoxville (June 8, 2017). "Paleoindian Period: Overview". New Georgia Encyclopedia (University System of Georgia). Retrieved November 9, 2018.{{cite web}}: CS1 maint: multiple names: authors list (link)

External links

This page was last edited on 26 October 2023, at 11:36
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.