2.2 – Minerals.

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Presentation transcript:

2.2 – Minerals

Do Now What are the four major processes by which minerals form?

Do Now What are the four major processes by which minerals form? Crystallization from magma Precipitation Changes in pressure and temperature Formation from hydrothermal solutions.

Key Words Composition Inorganic

Vocab Words Mineral Silicate Silicon-Oxygen Tetrahedron

Minerals Almost everything that is manufactured contains minerals. The lead in your pencil is a mineral called graphite. Salt grains are table salt which is sodium chloride. Drinking glasses are mostly made of quartz.

Minerals A mineral is a naturally occurring, inorganic solid with an orderly structure and a definite chemical composition. For an Earth material to be considered a mineral, it must have the following characteristics: Naturally occurring, formed by natural geologic process. Solid substance Orderly crystalline structure Definite chemical composition Generally considered inorganic

How Minerals Form Minerals form nearly everywhere on Earth under different conditions. There are four major processes by which minerals form: Crystallization from magma Precipitation Changes in pressure and temperature Formation from hydrothermal solutions

Crystallization from Magma Magma is molten rock and it forms deep within Earth. As magma cools, elements combine to form minerals. Feldspar Quartz Muscovite Hornblende

Precipitation The water in Earth’s lakes, rivers, ponds, oceans, and beneath its surface contains many dissolved substances. If this water evaporates, some of the dissolved substances can react to form minerals. Limestone Halite Calcite

Pressure and Temperature Some minerals, including talc and muscovite, form when existing minerals are subjected to changes in pressure and temperature. An increase in pressure can cause a mineral to recrystallize while still solid. The atoms are simply rearranged to form more compact minerals.

Hydrothermal Solutions A hydrothermal solution is a very hot mixture of water and dissolved substances. When these solutions come into contact with existing minerals, chemical reactions take place to form new minerals. Bornite Chalcopyrite

Mineral Groups Common minerals, together with the thousands of others that form on Earth, can be classified into groups based on their composition. Silicates Carbonates Oxides Sulfates and Sulfides Halides Native Elements

Silicates The most common groups of minerals on Earth. The two most abundant elements in Earth’s crust are silicon and oxygen. Silicon and oxygen combine to form a structure called the silicon-oxygen tetrahedron. Consists of one silicon atom and four oxygen atoms, provides the framework of every silicate mineral. Except for a few silicate minerals, such as pure quartz (SiO2), most silicates also contain one or more other elements.

Carbonates Second most common mineral groups. Minerals that contain the elements carbon, oxygen, and one or more other metallic elements Calcite is the most common; dolomite, limestone and marble are also examples.

Oxides Minerals that contain oxygen and one or more elements, which are usually metals. Some oxides, including the mineral called rutile (TiO2), form as magma cools deep beneath Earth’s surface. Ex: Hematite, Corundum and Rutile

Sulfates and Sulfides Sulfates and sulfides are minerals that contain the element sulfur. Ex: Anhydrite, Gypsum Sulfides are minerals that contain the element galena. Ex: Sphalerite, Pyrite

Haildes Minerals that contain a halogen ion plus one or more other elements. Ex: Fluorine, Chlorine, Halite Forms when salt water evaporates

Native Elements Minerals that exist in relatively pure form. Ex: Gold, Silver, Copper, Sulfur and Carbon

Group Challenge Question Fill out this chart and place in your group folders. Different Ways Minerals Form What Happens in This Process? Examples of Minerals Formed This Way