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Charlie–Gibbs fracture zone is a system of two parallel fracture zones. It is the most prominent interruption of the Mid-Atlantic Ridge between the Azores and Iceland , with the longest faults in the North Atlantic, and is ecologically an important biosystems boundary.
The Charlie-Gibbs fracture zone consists of two fracture zones in the North Atlantic that extend for over 2,000 km (1,200 mi). These fracture zones displace the Mid-Atlantic Ridge a total of 350 km (220 mi) to the west. The section of the Mid-Atlantic Ridge between the two fracture zones is seismically active. [6]
Fracture zones are much longer than wide, but may have feature complexity within their width. ... Charlie-Gibbs fracture zone [3] 2000: 350 [8
A more definitive mapping of fracture zones, including many with no official name, or not meeting the criteria for inclusion on this map, based on the 2015 project of Wessel et al., [1] exists as of 2018. [2]. This page is used on multiple pages and has complex logic so any alteration should be checked as a minor typo can break display on ...
As the water flows southward at the bottom of the channel, it entrains surrounding water of the eastern North Atlantic, and flows to the western North Atlantic through the Charlie–Gibbs fracture zone, entraining with LSW. This water is less dense than DSOW and lays above it as it flows cyclonically in the Irminger Basin.
For a leading man in a massive series, Mark Harmon got to play Special Agent Leroy Jethro Gibbs as a bit of a man of mystery on the “NCIS” franchise mothership series, at least up to the point ...
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In July 1968, Josiah Willard Gibbs surveyed a large fracture zone crossing the Mid-Atlantic Ridge at This fracture zone was known at the time as Charlie Fracture Zone, after the United States Coast Guard ' s Ocean Weather Station Charlie at 52°45′N 35°30′W / 52.750°N 35.500°W / 52.750; -35.500