Parts of molten rock at mid-ocean ridges are Magnetic minerals.
Further Explanations:
Mid-ocean ridges are defined as the seafloor mountain formed by the tectonic movement of the plates found in depth of 2,600 meters. And can rise up to 2km above the deepest ocean basin. This process takes place at the divergent plate boundary. The rate at which the spreading of the seafloor takes place concludes the morphology of the crest and width of the ocean basin. The new seafloor and the oceanic floor thus formed is the result of plate separation and mantle upwelling. The molten magma rises up from the faults in the form of lava and then form a new oceanic crust which on cooling forms lithosphere.
Magnetic mineral that have erupted during the volcanic eruption can be defined as the mineral that have magnetic properties. These minerals are generally obtained from the lava that has erupted during the volcanic eruption. These magnetic minerals also have the tendency to create a magnetic field around the region where it exists.
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1.what layers of earth make up the lithosphere answers Details?
2.what resource can best help you learn about the terrain in a particular area before you arrive?
3.which of the following is not true about sedimentary rocks? a. they are formed through compaction and cementation. c. they are formed from igneous rock fragments. b. they are made up of sediments. d. they are not part of the rock cycle?
Answer Details:
Grade: High School
Subject: Geography
Chapter: Mineralogy
Keywords: Mid-ocean ridges, tectonic movement, ocean basin, seafloor, morphology, plate, separation, mantle, upwelling.Magnetic properties, volcanic eruption
