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Τι (ποιος) είναι J-Anomaly Ridge - ορισμός
J-Anomaly Ridge
The J-Anomaly Ridge is a bathymetric feature in the North Atlantic Ocean, extending southwest from the eastern end of the Grand Banks of Newfoundland. It has a length of about and rises above the general level of the Sohm Abyssal Plain.
ridge
![The edges of [[tuya]]s can form ridges.](https://commons.wikimedia.org/wiki/Special:FilePath/The Table1.jpg?width=200 "The edges of [[tuya]]s can form ridges.")
![knife-edge ridge]] towards the [[pyramidal peak]]s [[Vihren]] and [[Kutelo]]](https://commons.wikimedia.org/wiki/Special:FilePath/Vihren Pirin IMG 0859.jpg?width=200 "knife-edge ridge]] towards the [[pyramidal peak]]s [[Vihren]] and [[Kutelo]]")
GEOLOGICAL FEATURE CONSISTING OF A CHAIN OF MOUNTAINS OR HILLS THAT FORM A CONTINUOUS ELEVATED CREST FOR SOME DISTANCE
Ridges; Ridge-line; Ridgeline; Ridge (geology); Stratigraphic ridge; Crest line; Hill ridge; Mountain ridge; Ridge of hills; Main chain; Mountain crest; Ridge line; Reef (geomorphology); Spur (geology)
¦ noun
1. a long, narrow hilltop, mountain range, or watershed.
the edge formed where the two sloping sides of a roof meet at the top.
2. a narrow raised band on a surface.
a raised strip of arable land, especially one of a set separated by furrows.
3. Meteorology an elongated region of high barometric pressure.
¦ verb [often as adjective ridged] mark with or form into ridges.
Derivatives
ridgy adjective
Origin
OE hrycg 'spine, crest', of Gmc origin.
Free-air gravity anomaly
In geophysics, the free-air gravity anomaly, often simply called the free-air anomaly, is the measured gravity anomaly after a free-air correction is applied to account for the elevation at which a measurement is made. It does so by adjusting these measurements of gravity to what would have been measured at a reference level, which is commonly taken as mean sea level or the geoid.
