79:, Boa Vista, Nola and Senghor. The third and fourth are named after explorers of Cape Verde, the other, the founding father of Senegal. The highest point is 2,220 meters below sea level and the deepest is in the range of over 3,000 meters deep. In the east end of the rise is the Dakar Canyon. It ranges between the 14 and the 22Β° parallels north and is 900 km long. Near the rise is the westernmost point in Africa,
178:) of the Northern Hemisphere. Humpback whales migrate annually from the North Sea to winter around Cape Verde from January to mid-May. The humpback whale population became limited due to severe overfishing during the 19th century and, although the total North Atlantic population of humpbacks had rebounded to more than 10,000 individuals by 1993, the Cape Verde population remained uncertain as of 2009.
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and the ODP 659. At the DSDP 368 location which was drilled 985 meters deep, it is divided into three units, the first unit composes of marls and oozes, the second composes of turbidites and the third composes of black shales, they lie above pelagic limestones and the oceanic crust. In that area
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era in the area what is now the east of the rise, around 131 to 128 million years ago, the seamounts of Maio and
Santiago were formed, at the time they were closer to the Mid-Atlantic Ridge. The spreading rate was slow and moved a centimeter a year.
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In the waters above the rise, eighteen species of whales and dolphins have been recorded in the waters of the Cape Verde archipelago. The area is cited as one of two known breeding grounds for the humpback whale
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In the rise there are 13 smaller fracture zones, three extends as far as the Cape Verde Basin and another extends north into the Canary Basin and within the Canary
Islands.
288:"Seasonality of humpback whale Megaptera novaeangliae (Borowski, 1781) records in Cape Verde seas: eviden ce for the occurrence of stocks from both hemispheres?"
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Nola
Seamount may be the tallest seamount within Cape Verde with its elevation ranging from 60β70 meters deep, and probably the Cape Verde Rise.
251:"Recent data on whales and dolphins (Mammalia: Cetacea) from the Cape Verde Islands, including records of four taxa new to the ar chipelago"
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to the south. Numerous seamounts are located in the rise including the Cape Verde (or Cabo Verde) (Latin: sometimes as
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Between 15 and 7 million years ago, they were volcanically active. Its only volcanic activities in the basin are in
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A seismological investigation of the Fogo volcano, Cape Verde
Islands: Preliminary results
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to the north and the
Equatorial Atlantic Current around the south of the rise.
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208:. Vol. 147. London: Journal of the Geological Society. pp. 851β857.
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Molluscs (Mollusks) in the deep waters within the Cape Verde islands include
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and the
Cadamosto Seamount. Brava's last eruption was in the Holocene era.
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Over 1,500 km west of the rise are two fracture zones located at the
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are five basaltic sills. DSDP 368 is east of the island of Boa Vista.
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and the areas north and east of the islands and west of the
African
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Mitchell, J. G.; Le Bas, M.J.; Zielonka, J.; Furnes, H. (1983).
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The oldest rocks dates back to 155 million years ago during the
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Map of the
Atlantic Ocean featuring the Cape Verde Rise
223:. Earth and Planetary Science Letters. pp. 61β76.
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Fracture zones across the Cape Verde Rise, NE Atlantic
238:. Vol. 20. Volcanol. Seismol. pp. 199β217.
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On dating the magmatism of Maio, Cape Verde
Islands
187:at depths between 273 m and 970 m below sea level.
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Description of the Cape Verde Rise at DSDP 368 area
83:, northwest of the rise is the Santo AntΓ£o Ridge.
136:, two research drillings were done so far, the
86:In the waters above the Cape Verde Rise is the
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286:Hazevoet, Cornelius J.; et al. (2011).
249:Hazevoet, Cornelis J.; et al. (2010).
234:Heleno, S.I.N.; Fonseca, J.F.D.B. (1999).
31:is an oceanic feature that includes the
16:Prominence on the Atlantic Ocean surface
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88:Canary (or Canarian) Current
63:The rise are bounded by the
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204:Williams, C.A.U. (1990).
130:Deep Sea Drilling Project
176:Megaptera novaeangliae
134:Ocean Drilling Program
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295:Zoologia Caboverdiana
258:Zoologia Caboverdiana
128:In the course of the
75:being off the cape),
67:to the north and the
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124:Deep sea exploration
184:Tiberia apicifusca
103:Mid-Atlantic Ridge
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33:Cape Verde Islands
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37:Continental Shelf
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301:(2): 25β29.
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39:as well as
191:References
41:Mauritania
307:2074-5737
270:2074-5737
77:Cadamosto
59:Geography
321:Category
138:DSDP 368
132:and the
81:Cap-Vert
145:Geology
45:Senegal
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109:, the
105:, the
291:(PDF)
254:(PDF)
169:Fauna
163:Brava
303:ISSN
266:ISSN
159:Fogo
113:and
107:Kane
43:and
27:The
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