List of fracture zones

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.

Major fractures zones of the Atlantic can be seen on this ocean depth map

Pacific Ocean

Major Pacific trenches (1–10) and fracture zones (11–20): 1. Kermadec 2. Tonga 3. Bougainville 4. Mariana 5. Izu–Ogasawara 6. Japan 7. Kuril–Kamchatka 8. Aleutian 9. Middle America 10. Peru–Chile 11. Mendocino 12. Murray 13. Molokai 14. Clarion 15. Clipperton 16. Challenger 17. Eltanin 18. Udintsev 19. East Pacific Rise (S-shaped) 20. Nazca Ridge

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 host 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.

Chile Rise

The fracture zones of the Chile Rise trend in a west to east fashion with the most southern ones taking a slightly more southwest to northeast orientation. This non-perpendicular relation to Chile's 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 make up large sections of the Nazca-Antarctic Plate boundary.

Map of the Chile Rise and its fracture zones in Nazca and the Antarctic Plates
NameMinimum length
in km
Length of transform
boundary in km
Position at Ridge
Chile2,250 (1,400)1,100 (680)35°32′24″S 104°37′3″W
Chiloé1,750 (1,090)50 (30)42°59′43″S 83°11′5″W
Darwin50 (30)45°54′29″S 76°25′31″W
Desolación0
Esmeralda049°06′47″S 80°12′33″W
Guafo1,550 (960)280 (170)44°47′55″S 80°15′53″W
Guamblin1,300 (810)70 (40)45°44′7″S 77°27′32″W
Madre de Dios0
Mocha450 (280)039°14′24″S 77°22′59″W
Taitao0
Tres Montes0
Valdivia2,100 (1,300)650 (400)41°23′25″S 87°23′36″W

East Pacific Rise

NameMinimum length
in km
Length as plate
boundary in km
Coordinates
Easter
Mendaña0
Nazca019°49′28″S 77°35′53″W
Quiros0

Galapagos Rise

Juan de Fuca and Gorda Ridges

Molokai and Murray fracture zones shown in the list were created by ridge segments that no longer exist.

A map of the Juan de Fuca Plate

Atlantic Ocean

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 kilometres (34 mi):[1] two for each degree of latitude. Physically it makes sense to group Atlantic fracture zones into three categories:[2]

  1. Small offset: length of transform fault less than 30 kilometres (19 mi)
  2. Medium offset: offset over 30 kilometers
  3. Large offset: offset several hundreds of kilometers

Mid-Atlantic Ridge (Northern Hemisphere)

NameMinimum length
in km
Length of
transform fault in km
Position at Ridge
Saint Paul[3]14514540.661°N 27.931°W / 0.661; -27.931
Saint Peter[3]333402.532°N 31.008°W / 2.532; -31.008
Strakhov[3] (formerly:Four North[4])18141003.933°N 32.116°W / 3.933; -32.116
Sierra Leone[3]1111526.230°N 33.588°W / 6.230; -33.588
Bogdanov[3]173847.135°N 34.351°W / 7.135; -34.351
Vernadsky[3]1941077.693°N 37.483°W / 7.693; -37.483
Doldrums[3]3811448.119°N 38.750°W / 8.119; -38.750
Arkhangelskiy[3]691998.855°N 39.938°W / 8.855; -39.938
Vema[3]82230010.726°N 42.333°W / 10.726; -42.333
Mercurius[5]3912.132°N 43.924°W / 12.132; -43.924
Marathon[5]7812.611°N 44.430°W / 12.611; -44.430
Fifteen Twenty, also known
as Barracuda or Cabo Verde[3]
1195195[5]15.320°N 45.871°W / 15.320; -45.871
Vidal[2]5017.832°N 46.589°W / 17.832; -46.589
Luymes South[2]3018.541°N 46.465°W / 18.541; -46.465
Luymes North[2]2418.967°N 46.128°W / 18.967; -46.128
Snellius[2]4120.616°N 45.756°W / 20.616; -45.756
Kane[3]1040150[6]23.718°N 45.583°W / 23.718; -45.583
Northern[2]1040925.689°N 45.193°W / 25.689; -45.193
Tyro[2]1529.365°N 43.007°W / 29.365; -43.007
Atlantis[3]8436630.068°N 42.372°W / 30.068; -42.372
Cruiser[2]932.323°N 40.195°W / 32.323; -40.195
Charis[2]1333.059°N 39.628°W / 33.059; -39.628
Hayes[3]62415133.615°N 38.439°W / 33.615; -38.439
Oceanographer[3]75114835.149°N 35.562°W / 35.149; -35.562
Tydeman2136.641°N 33.464°W / 36.641; -33.464
Pico (to the west)[2][3]7196737.468°N 31.899°W / 37.468; -31.899
East Azores (to the east)[2][3]7586737.468°N 31.899°W / 37.468; -31.899
Kurchatov[3]1742040.537°N 29.456°W / 40.537; -29.456
Petrov[3]74940.537°N 29.456°W / 40.537; -29.456
Maxwell[3]2147.636°N 27.527°W / 47.636; -27.527
Faraday[3]5062349.711°N 28.636°W / 49.711; -28.636
Charlie-Gibbs[3]2000350[2]52.624°N 33.198°W / 52.624; -33.198
Bight[3]3362356.721°N 33.792°W / 56.721; -33.792
Jan Mayen[3]37421171.372°N 9.405°E / 71.372; 9.405
Greenland (to the west)[7]036574.04°N 8.82°E / 74.04; 8.82
Senja (to the east)[7]039874.04°N 8.82°E / 74.04; 8.82

Fracture zones involved in the early opening of the North Atlantic

American sideAfrican side
Hudson Fracture Zone
Snorri Fracture Zone
Cartwright Fracture Zone
Julian Haab Fracture Zone
Minna Fracture Zone
Leif Fracture Zone
Newfoundland Fracture Zone[8]
Kelvin Fracture Zone[9]Canary Fracture Zone[9]
Cape Fear Fracture Zone[9]Cape Verde Fracture Zone[9]
Bahama Fracture Zone[9]Guinea Fracture Zone[9]

Mid-Atlantic Ridge (Southern Hemisphere)

NameMinimum length
in km
Length of
transform fault in km
Position at Ridge
Romanche[3]24459500.49°S 20.49°W / -0.49; -20.49
Chain[3]13152691.213°S 14.229°W / -1.213; -14.229
Ascension[3]11492646.928°S 12.283°W / -6.928; -12.283
Bode Verde[3]301823211.686°S 13.936°W / -11.686; -13.936
Cardno[3]16498714.076°S 14.056°W / -14.076; -14.056
Tetyaev[3]81012216.271°S 13.719°W / -16.271; -13.719
Saint Helena[3]11841916.617°S 14.344°W / -16.617; -14.344
Hotspur[3]144611317.721°S 13.329°W / -17.721; -13.329
Martin Vaz[3]13242618.594°S 12.633°W / -18.594; -12.633
Rio Grande[3]177415629.081°S 13.067°W / -29.081; -13.067
Tristan Da Cunha[3]10142638.388°S 16.796°W / -38.388; -16.796
Gough[3]10574240.637°S 16.637°W / -40.637; -16.637
Conrad (to the west)[3]316055.185°S 0.133°W / -55.185; -0.133
Bouvet (to the east)[3]198055.185°S 0.133°W / -55.185; -0.133

Indian Ocean

Southwest Indian Ridge

Carlsberg Ridge

Central Indian Ridge

  • Mauritius

Lakshadweeo-Chagos Ridge

  • Vishnu

Southern Ocean

References

  1. Gilman, Larry; Lerner, K. Lee. "Mid-Ocean-Ridges". Water Encyclopedia. Retrieved 2011-11-29.
  2. Müller, R. Dietmar; Roest, Walter R. (1992). "Fracture Zones in the North Atlantic from Combined Geosat and Seasat Data" (PDF). Journal of Geophysical Research. 97 (B3): 3337–50. Bibcode:1992JGR....97.3337M. doi:10.1029/91JB02605. Archived from the original (PDF) on 2012-03-28. Retrieved 2011-11-30.
  3. Name from GEBCO gazetteer, position refined by means of etopo2 and sample data of GPlates
  4. Udintsev, G.B. (1996). "Equatorial Segment of the Mid-Atlantic Ridge". Unesco. Archived from the original on 2012-09-07. Retrieved 2011-12-05.
  5. Roest, W. R.; Collette, B. J. (1986). "The Fifteen Twenty Fracture Zone and the North American – South American plate boundary". Journal of the Geological Society. 143: 833–43. doi:10.1144/gsjgs.143.5.0833.
  6. Tucholke, Brian E.; Schouten, Hans (1988-03-01). "Kane Fracture Zone". Marine Geophysical Research. 10: 1–39. Bibcode:1988MarGR..10....1T. doi:10.1007/BF02424659.
  7. "Map with Jan Mayen, Greenland and Senja Fracture Zones". Ocean Drilling Project. Retrieved 2011-12-16.
  8. Auzende, J.M.; Olivet, J.L.; Bonnin, J. (1970). "Marge du Grand Bank et la fracture de Terre-Neuve". Compt. Rend. (in French). 271: 1063–66.
  9. Le Pichon, Xavier; Fox, Paul J. (1971-09-10). "Marginal Offsets, Fracture Zones, and the Early Opening of the North Atlantic". Journal of Geophysical Research. 76 (26): 6294–308. Bibcode:1971JGR....76.6294L. doi:10.1029/JB076i026p06294.
  10. Patriat, P., Sauter, D., Munschy, M., & Parson, L. (1997). A survey of the Southwest Indian Ridge axis between Atlantis II Fracture Zone and the Indian Ocean Triple Junction: Regional setting and large scale segmentation. Marine Geophysical Researches, 19(6), 457–80.
Sources
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