1.It is extrusive volcanic rock
2.it white,grey or black in color
3.it has fine grained or aphanatic texture
Rhyolitic magma is typically formed from the melting of continental crust rocks such as granite and other felsic rocks. These rocks have high silica content, which contributes to the high viscosity of rhyolitic magma. Magma properties can also be influenced by other factors such as water content and temperature.
Lava domes are large geological features created by rhyolitic magma. Rhyolitic magma promotes plinian eruptions. Plinian eruptions can happen very quickly and shoot lave several miles into the air.
basaltic,andesitic,rhyolitic
Yes, rhyolitic magmas are several hundred °C colder than basaltic magmas. This is because the melting point of a rhyolitic magma is much lower than that of basaltic magma. Instead of heating up rhyolitic magma much above its melting point it will ascend and either crystallize in the Earth's interior as a pluton or erupt.
Basaltic, Andersitic, and Rhyolitic
The opposite of basaltic is rhyolitic. Basaltic rocks are formed from lava that is low in silica content, while rhyolitic rocks are formed from lava that is high in silica content.
Basaltic, andesitic and rhyolitic
Not necessarily. It is often andesitic or rhyolitic.
Both rhyolitic and basaltic lava flows have been found in the Yellowstone Caldera. There are alro large deposits of rhyolitic tuff.
The three types of magma, named for the rock they form are basaltic, rhyolitic and andesitic. Rhyolitic magma is rich in silica and water vapor.
Scientists measure the silica content, temperature, and viscosity of magma to classify it into different types, such as basaltic, andesitic, or rhyolitic. These properties help determine how explosive or effusive a volcano might be when the magma erupts.
Yes. It is not uncommon for rhyolitic material to form pyroclastic flows.