no it does not not at all it takes about well the longest would ever be 10 to 20 years
It will for an intrusive igneous rock. They usually take longer to cool and have more coarse grains.
It will for an intrusive igneous rock. They usually take longer to cool and have more coarse grains.
Practically all petrifaction takes a million years or more. However, formation by silicates can take less than 50,000 years. Some examples are estimated to be between 50 to 250 million years old.
No. Whether igneous rocks cool quickly or slowly is more dependent on whether the rock is intrusive or extrusive than whether it is mafic or felsic. Because it is so viscous it is often difficult for felsic magma to erupt, and so it is more likely to be intrusive and thus cool slowly. When felsic magma is involved in an eruption, it often erupts explosively. Some of the molten rock ejected cools extremely rapidly, forming volcanic glass.
The mid-Atlantic ridge has been constantly producing more new land as magma is pushed up into the crack and hardens. This pushes apart the North American and Eurasian tectonic plates.
Elberton granite began 325 million years ago as a large mass of magma or molten rock. The magma rose upward and came to rest about nine miles beneath Elberton. There it cooled very slowly -- taking more than a million years -- and solidified into granite. That was more than 300 million years ago. Since then, the granite has been pushed upward, and the land above it has been removed by erosion.
Magma is molten rock that is below ground level so it probably wouldn't be exposed to the open air.
No. They would contain fewer, but larger mineral crystals when compared to igneous rocks which have cooled quickly from lava or magma.
Magma in the mantle moves in a current called a convection current. A convection current is a circular flow of a substance in which a hot substance rises, cools, sinks, gets hot again, and repeats. In this way, magma in the mantle flows in currents of more hot or more cool magma.
a million or more years
Anything that is warmer than its surroundings will transfer heat to them and cool down in the process. Lava from a volcano transfers heat to the air, which then carries it away. Underground magma transfers heat to the surrounding rock. Since rock is a poor conductor of heat the magma will cool much more slowly than if it were at the surface.
When it is heated it becomes less dense (i.e. lighter). The more dense (i.e. heavier) magma sinks while the less dense magma rises to the top. It will eventually cool again causing a convection current within the mantle.
Pi has more than a million digits to it. Its 3.14159...etc
Geologic time is very long, so a million or more years is the best choice.
As old as history itself, at least a few million years.
Millions of million years, Billions of years, (Aeon).
The sun was roughly 4.6 billion years old a million years ago. The margin for error on the estimated age of the sun is more than a million years.