Fracture zones are common features in the geology of oceanic basins. Globally most fault zones are located on divergent plate boundaries on oceanic crust. This means that they are located around mid-ocean ridges and trend perpendicular to them. The term fracture zone is used almost exclusively for features on oceanic crust, similar structures on continental crust are instead termed transform or strike slip faults, a denomination active fracture zones also can have. Some fracture zones have been created by mid-ocean ridge segments that have been subducted and may not longer exist.
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Most fracture zones in the Pacific Ocean originate from large mid-ocean ridges (also called "rises") such as the East Pacific Rise, Chile Rise and Juan de Fuca Ridge. The plates that hosts the fractures are Nazca, Pacific, Antarctic, Juan de Fuca and Cocos among others. Fracture zones being subducted under Southern and Central America are generally southwest-northeast oriented reflecting the relative motion of Cocos, Nazca and the Antarctic Plates.
The fracture zones of the Chile Rise trends in a west to east fashion with the most southern ones taking a slightly more southwest to northeast orientation. This non perpendicular relation to Chiles coast reflects the oblique subduction of Nazca Plate under southern Chile. West of Chile rise the fracture zones are hosted in the Antarctic Plate. Some fracture zones such as Chile and Valdivia makes up large sections of the Nazca-Antarctic Plate boundary.
Name | Minimum length in km |
Length as plate boundary in km |
Coordinates |
---|---|---|---|
Chile | 2250 | 1100 | |
Chiloé | 1750 | 50 | |
Darwin | 50 | ||
Desolación | 0 | ||
Esmeralda | 0 | ||
Guafo | 1550 | 280 | |
Guamblin | 1300 | 70 | |
Madre de Dios | 0 | ||
Mocha | 450 | 0 | |
Taitao | 0 | ||
Tres Montes | 0 | ||
Valdivia | 2100 | 650 |
Name | Minimum length in km |
Length as plate boundary in km |
Coordinates |
---|---|---|---|
Easter | |||
Mendaña | 0 | ||
Nazca | 0 | ||
Quiros | 0 |
Molokai and Murray fracture zones shown in the list were created by ridge segments that no longer exist.
In the Atlantic Ocean most fracture zones originate from the Mid-Atlantic Ridge, which runs from north to south, and are therefore west to east oriented in general. There are about 300 fracture zones, with an average north-south separation of 55 kilometers[1]: two for each degree of latitude. Physically it makes sense to group Atlantic fracture zones into three categories[2]:
Name | Minimum length in km |
Length of transform fault in km |
Position at Ridge |
---|---|---|---|
Saint Paul[3] | 1451 | 454 | |
Saint Peter[3] | 333 | 40 | |
Strakhov[3] (formerly:Four North[4]) | 1814 | 100 | |
Sierra Leone[3] | 1111 | 52 | |
Bogdanov[3] | 173 | 84 | |
Vernadsky[3] | 194 | 107 | |
Doldrums[3] | 381 | 144 | |
Arkhangelskiy[3] | 691 | 99 | |
Vema[3] | 822 | 300 | |
Mercurius[5] | 39 | ||
Marathon[5] | 78 | ||
Fifteen Twenty, also known as Barracuda or Cabo Verde[3] | 1195 | 195[5] | |
Vidal[2] | 50 | ||
Luymes South[2] | 30 | ||
Luymes North[2] | 24 | ||
Snellius[2] | 41 | ||
Kane[3] | 1040 | 150[6] | |
Northern[2] | 1040 | 9 | |
Tyro[2] | 15 | ||
Atlantis[3] | 843 | 66 | |
Cruiser[2] | 9 | ||
Charis[2] | 13 | ||
Hayes[3] | 624 | 151 | |
Oceanographer[3] | 751 | 148 | |
Tydeman | 21 | ||
Pico (to the west)[3][2] | 719 | 67 | |
East Azores (to the east)[3][2] | 758 | 67 | |
Kurchatov[3] | 174 | 20 | |
Petrov[3] | 74 | 9 | |
Maxwell[3] | 21 | ||
Faraday[3] | 506 | 23 | |
Charlie-Gibbs[3] | 1020 | 350[2] | |
Bight[3] | 336 | 23 | |
Jan Mayen[3] | 374 | 211 | |
Greenland (to the west)[7] | 0 | 365 | |
Senja (to the east)[7] | 0 | 398 |
American side | African side |
---|---|
Newfoundland Fracture Zone[9] | |
Kelvin Fracture Zone | Canary Fracture Zone |
Cape Fear Fracture Zone | Cape Verde Fracture Zone |
Bahama Fracture Zone | Guinea Fracture Zone |
Name | Minimum length in km |
Length of transform fault in km |
Position at Ridge |
---|---|---|---|
Romanche[3] | 2445 | 950 | |
Chain[3] | 1315 | 269 | |
Ascension[3] | 1149 | 264 | |
Bode Verde[3] | 3018 | 232 | |
Cardno[3] | 1649 | 87 | |
Tetyaev[3] | 810 | 122 | |
Saint Helena[3] | 1184 | 19 | |
Hotspur[3] | 1446 | 113 | |
Martin Vaz[3] | 1324 | 26 | |
Rio Grande[3] | 1774 | 156 | |
Tristan Da Cunha[3] | 1014 | 26 | |
Gough[3] | 1057 | 42 | |
Conrad (to the west)[3] | 316 | 0 | |
Bouvet (to the east)[3] | 198 | 0 |
The Global Seafloor Fabric and Magnetic Lineation Data Base Project