Magma that has bubbled up through the crack in the Earth's surface.
It pushes the tectonic plates that meet at the ridge apart.
While it is molten it is above the Curie temperature and is not magnetic, as it cools below this temperature the ambient magnetic field becomes "frozen" into the basalt.
shakes
linear
rift valley
A medial moraine.
accorsing to the earths magnetic field
While it is molten it is above the Curie temperature and is not magnetic, as it cools below this temperature the ambient magnetic field becomes "frozen" into the basalt.
accorsing to the earths magnetic field
The color of rocks that forms the oceanic crust at the Mid Ocean Ridge are dark (blackish) color and they are dense and ferromagnetic in property. The major rock type is Basalt.
The molten material then spreads out, pushing the older rock to both sides of the ridge. As the molten material cools, it forms a strip of solid rock in the center of the ridge. Then more molten material flows into the crack. The material splits apart the strip of solid rock that formed before, pushing it aside.
Basalt is extruded from volcanoes and MOR (mid ocean ridges). It actually forms in the earth's mantle and just solidifies on the earth's surface.
Basalt is a dark-colored igneous rock that forms when low-silica lava cools on Earth's surface. It may commonly have vesicles. It often forms two types of lava flow: pahoehoe with smooth surfaces and a'a with rough surfaces. Basalt is commonly formed at mid-ocean ridges, oceanic hot spots, and in continental flood basalts.
Basalt is an extrusive, volcanic rock. It commonly forms the volcanic mountains found in the Oceans - eg Hawaii is made of basalts.
true
pillow lava named that because when it cools it looks like pillows.
New oceanic crust is created along mid ocean ridges. These are areas of the earth where there is divergence or splitting of the ocean floor and basaltic magma oozes out from within the mantle to occupy the gaps and form new crusts.
it forms Basalt.