no.
a molten rock
They may contain naturally occurring magnetic minerals.
They have the electromagnetic force in which two objects are attracted to one another in a specific field or range. It happens usually when the rocks contain iron which is the most important magnetic material.
three are : eruptions of molten material magnetic stripes in the rock of the ocean floor and the ages of the rocks themselves :)
three are : eruptions of molten material magnetic stripes in the rock of the ocean floor and the ages of the rocks themselves :)
Yes, molten rock material from which minerals can crystallize is called magma when it is below the Earth's surface. Once the molten rock material reaches the Earth's surface, it is referred to as lava.
magma
Basalt itself is not inherently magnetic, but it can contain magnetic minerals such as magnetite. These minerals can make some basaltic rocks exhibit magnetism, especially when they have been cooled from molten lava. The magnetic properties of basalt can also be influenced by the conditions under which it formed and the presence of other minerals. Overall, while basalt can have magnetic characteristics, it is not universally magnetic.
Sedimentary rocks, such as shale, sandstone, and limestone, are most likely to contain fossils. These rocks form from the accumulation of sediment and often preserve the remains of plants and animals. Fossils are less commonly found in igneous and metamorphic rocks, as these rocks form from molten material and intense pressure and heat, which usually destroy any existing fossils.
Igneous rock is formed from the solidification of molten material, such as lava or magma. This process can occur either above or below the Earth's surface and results in rocks like basalt, granite, and obsidian.
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.
Felsic rocks are light-colored, rich in silica and aluminum, and have high viscosity when molten. They contain minerals such as quartz and potassium feldspar. Mafic rocks are dark-colored, rich in magnesium and iron, have low viscosity when molten, and contain minerals like olivine and pyroxene.