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Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

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Page 1: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

BellringerWhat happens to the oldest islands in a volcanic

island chain created by a mantle hot spot?

Page 2: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Properties of Magma

Notes

Page 3: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Physical and Chemical Properties•Like other substances, magma is made up of

elements and compounds, and has a certain set of properties, or traits. Properties can be physical or chemical.

•An element is a substance that cannot be broken down into other substances. Carbon, Oxygen, Argon, Gold, Tin, Lead, etc.

•A compound is a substance made of two or more elements that have been chemically combined. Water, Carbon Dioxide, Table Salt, Sulfuric Acid, etc.

Page 4: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Elements Compounds

C

O

H

Page 5: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Physical and Chemical Properties•Physical properties are traits that

can be observed without changing what a substance is made of. Examples of physical properties are hardness, color, density, melting point, boiling point, and magnetism.

•Water, under normal pressure, will always have a melting point of 0°C and a boiling point of 100°C.

Page 6: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Physical and Chemical Properties• Chemical properties are traits that can be

observed only by changing what a substance is made of. Examples of chemical properties is a substances ability to burn and its ability to combine, or react, to another substance.

• You can often tell if a substance has reacted to another substance if it changes color, produces a gas, or forms a new, solid substance (precipitate).

• Iron’s reaction with oxygen to produce rust is an example of a chemical property.

Page 7: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

What is Viscosity?

•Viscosity is a physical property of liquids. How well a liquid flows depends on its viscosity.

•A liquid with a high viscosity is thick. It flows very slowly. Honey and syrup have high viscosities.

•A liquid with low viscosity is thin. It flows very quickly. Water and Kool-Aid® have low viscosities.

•The greater the friction between the fluid’s particles, the higher the viscosity.

Page 8: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Video - Three different viscosities

http://upload.wikimedia.org/wikipedia/commons/b/b7/Viscosity.gif

Page 9: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Viscosity of Magma

•Silica is a common substance in Earth’s crust. Magma contains silica. Magma that contains more silica has higher viscosity.

•High-silica magma produces high-viscosity lava. This lava flows slowly.

•High-silica magma cools to form light-colored, felsic igneous rocks such as granite, pegmatite, and rhyolite.

Page 10: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Rhyolite Granite

Pegmatite

Page 11: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Viscosity of Magma

•Low-silica magma produces low-viscosity lava. This lava flows quickly.

•Low-silica magma cools to form dark-colored, mafic igneous rocks such as basalt and gabbro.

Page 12: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Basalt Gabbro

Page 13: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Viscosity of Magma•Hotter magma has lower viscosity than

cooler magma.

•Very hot magma produces lava called Pāhoehoe. Pāhoehoe has low viscosity. It flows quickly. It hardens into a rippled surface.

•Cooler magma produces lava called ʻaʻā. ʻAʻā has high viscosity. It flows slowly. It hardens into rough chunks.

Page 14: Bellringer What happens to the oldest islands in a volcanic island chain created by a mantle hot spot?

Pāhoehoe ʻAʻā

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Lava Type

Temperature ViscositySilica

ContentColor

RockExamples

Pāhoehoe HIGH LOW LOW DARKBasaltGabbro

ʻAʻā LOW HIGH HIGH LIGHTGraniteRhyolite

Pegmatite