Basaltic Magma: This type of magma is low in silica content and has a low viscosity. It is often associated with shield volcanoes and produces basaltic rocks.
Rhyolitic Magma: Rhyolitic magma has a high silica content and high viscosity. It is linked to explosive eruptions and forms rhyolite rocks.
Formation of Magma
Magma is formed through the process of partial melting, which occurs when rocks are subjected to high temperatures and pressure. This can happen due to the heat generated by the underlying mantle or by the addition of heat from tectonic activity.
Magma Chambers
Magma is often stored in underground reservoirs known as magma chambers. These chambers can range in size and are crucial in the formation of volcanic eruptions.
Study Guide
Key Concepts to Understand
Definition of magma and its role in the formation of igneous rocks.
The various types of magma and their characteristics.
The process of partial melting and how it leads to the formation of magma.
Identify and analyze forces responsible for changes in rotational motion and develop an understanding of the effect of rotational inertia on the motion of a rotating object (e.g., merry-go-round, spinning toy, spinning figure skater, stellar collapse [supernova], rapidly spinning pulsar).