People study all kinds of rocks. 

Some people study rocks. 
There are three main kinds of rocks. Some come from hot, melted stone. Some are made of tiny bits. Other rocks change from heat or weight.

Petrology is the study of rocks. 
First are igneous rocks. These form from magma, which is melted rock. These rocks can be volcanic or plutonic.
Second are sedimentary rocks. These are made of small pieces. These pieces come from other rocks or living things. They are held together in a fine material.
Third are metamorphic rocks. These rocks change from heat or pressure. They can start as any kind of rock. This original rock is called a protolith.
Some experts use a special way called experimental petrology. They use tools to make very high heat and pressure. This helps them study rocks from deep inside the Earth. They can even study rocks from the Moon. 
Petrology is a branch of geology that studies rocks. 
There are three main ways to group rocks. Igneous petrology studies rocks like granite or basalt. These rocks form when molten rock or magma cools down. Sedimentary petrology looks at rocks like sandstone or limestone. These rocks come from pieces of other rocks or biological deposits. They are often held together by a fine material. Metamorphic petrology studies rocks like marble or slate. These rocks change because of heat or pressure. The original rock is called a protolith.
Scientists use many tools to study these rocks. They use mineralogy to look at tiny minerals. They use petrography to see microscopic details. 
Some experts use a special method called experimental petrology. They use machines to create high heat and pressure. 
Petrology connects to many different parts of science. It uses chemistry to study what is inside a rock. It uses geophysics to study the Earth's physical properties. 
Petrology is a specialized branch of geology focused on the study of rocks. 
To understand rocks, petrologists use several scientific methods. They rely on mineralogy to identify the specific minerals within a sample. They also use petrography to study the microscopic details of a rock. 
Petrology is divided into three main branches based on rock types. The first is igneous petrology, which focuses on rocks like granite or basalt. These rocks form when molten rock, known as magma, crystallizes into a solid. Igneous rocks are further categorized as either volcanic or plutonic. The second branch is sedimentary petrology. This field studies rocks like sandstone, shale, or limestone. These rocks are made of particles from other rocks or biological and chemical deposits. These particles are usually held together in a matrix of finer material.
The third branch is metamorphic petrology. This branch studies rocks such as marble, slate, gneiss, or schist. These rocks change due to high temperature, high pressure, or both. The original rock that undergoes these changes is called a protolith. Any type of rock can serve as a protolith before it transforms. This transformation changes the rock's mineralogy, texture, or chemical makeup. Because of this, metamorphic petrology is often taught alongside igneous petrology. Both fields rely heavily on chemistry and the use of phase diagrams.
Some scientists specialize in experimental petrology to learn more about the deep Earth. These researchers use special apparatus to create very high temperatures and pressures. 
There are important distinctions between terms like lithology and petrography. In general use, lithology refers to describing rocks at a macroscopic scale. This means looking at large hand-samples or entire outcrops. Petrography, however, is the specialty that deals with microscopic details. In the petroleum industry, lithology has a more specific meaning. Workers use a process called mud logging to represent geological formations. As drilling occurs, cuttings are circulated out of the borehole. These cuttings are sampled and examined under a 10x microscope. They may also be tested chemically to understand the formation.
Petrology connects many different scientific disciplines together. It combines the study of physical matter with the study of chemical changes. The field uses the principles of geochemistry to understand the origins of rocks. It also uses geophysics to understand the Earth's physical properties. 
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