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http://geosciencemammino.wordpress.com/ Oceanic ridges

Diapositiva 1 · 2014. 3. 30. · Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of basalt (rich in iron and

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Page 1: Diapositiva 1 · 2014. 3. 30. · Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of basalt (rich in iron and

http://geosciencemammino.wordpress.com/

Oceanic ridges

Page 2: Diapositiva 1 · 2014. 3. 30. · Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of basalt (rich in iron and

Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of basalt (rich in iron and magnesium). It is thinner than continental crust. It is denser, having a mean density of about 3.0 grams per cubic centimeter as opposed to Continental which has a density of about 2.7 grams per cubic centimeter.

6 - 7 Km 35 Km

Page 4: Diapositiva 1 · 2014. 3. 30. · Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of basalt (rich in iron and

Oceanic ridges are found in every ocean basin and appear to girdle the Earth. The ridges rise from depths near 3 km and are roughly symmetrical in cross section. They can be thousands of Kilometres wide. In places, the crests of the ridges are offset across transform faults within fracture zones (Transform faults are those along which lateral movement occurs.)

The arrows show the direction of movement across the transform faults.

Page 5: Diapositiva 1 · 2014. 3. 30. · Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of basalt (rich in iron and

Spreading occurs as basaltic magma from the mantle rises into vertical tensional fractures in the lithosphere. This zone is constructive, as volcanism adds basalt rock to the lithosphere.

Page 6: Diapositiva 1 · 2014. 3. 30. · Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of basalt (rich in iron and

Oceanic ridges can be classified as slow (spreading up to 50 mm per year), intermediate (up to 90 mm per year), fast (up to 160 mm per year). Slow-spreading ridges are characterized by a rift valley at the crest. It is typically 1.4 Km deep and 20–40 km wide. Faster-spreading ridges lack rift valleys.

Page 8: Diapositiva 1 · 2014. 3. 30. · Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of basalt (rich in iron and

Map showing the age of Earth’s oceanic crust

Page 9: Diapositiva 1 · 2014. 3. 30. · Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of basalt (rich in iron and

Rising magma assumes the polarity of Earth’s geomagnetic field before it solidifies into oceanic crust. At spreading centres, this crust is separated into parallel bands of rock by successive waves of emergent magma. When Earth’s geomagnetic field undergoes a reversal, the change in polarity is recorded in the magma, which contributes to the alternating pattern of magnetic striping on the seafloor.

Seafloor spreading and magnetic striping

Page 12: Diapositiva 1 · 2014. 3. 30. · Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of basalt (rich in iron and

TASK

2- What is the mid-Atlantic ridge?

1- Make your labelled drawing of an oceanic ridge