12
http://pao.cnmoc.navy.mil/PAO/Educate/Oce anTalk2/indexnew.htm

Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm

Embed Size (px)

Citation preview

Page 1: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm

http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm

Page 2: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm

The sea floor is not a flat surface

Page 3: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm

Earthquake epicenters display a typically nonrandom distribution

Page 4: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm

Seismicity defines the plate boundaries

Page 5: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm

Pacific Pacific plateplate

Nazca Nazca plateplateAustralian Australian

plateplate

South South American American plateplate

North North American American plateplate

African African plateplate

Gorda Gorda plateplate

Cocos Cocos plateplate

Antarctic plateAntarctic plate

Philippine Philippine plateplate

Ind

ian

pla

teIn

dia

n p

late

Eurasian platesEurasian platesEurasian Eurasian platesplates

Caribbean Caribbean plateplate

Some major plates

Page 6: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm

The older the sea floor the farther it is from the ridge axis

0.0

9.6

20.2

33.0

40.2

47.9

56.0

68.7

83.0

118

.0

126

.513

1.7

141

.914

9.9

156

.6

180

.0

Age of the sea floor (Ma B.P.)

Page 7: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm
Page 8: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm
Page 9: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm
Page 10: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm
Page 11: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm
Page 12: Http://pao.cnmoc.navy.mil/PAO/Educate/OceanTalk2/indexnew.htm

A convergent plate boundary, e.g., the convergence of Nazca

and South American plates