Volcanoes Types of volcanoes ShieldLava pours from an

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Volcanoes • Types of volcanoes: Shield—Lava pours from an opening (called a vent) creating

Volcanoes • Types of volcanoes: Shield—Lava pours from an opening (called a vent) creating gently sloping sides, flat and round. Example: Mauna Loa (Hawaii) or Mauna Kea (page s 112 -113 red book)

Volcanoes Cinder cone—Created by an explosive eruption out of the ground creating steep sloping

Volcanoes Cinder cone—Created by an explosive eruption out of the ground creating steep sloping sides and a narrow base. This type can spew lava, cinders, ash and tephra (volcanic rocks). After erupting tends to be inactive and erodes easily. Example: Paricutin Mexico (page s 113 red book)

Volcanoes Composite—formed by layers of lava and tephra has steep slopes and broad bases,

Volcanoes Composite—formed by layers of lava and tephra has steep slopes and broad bases, also called Stratovolcanoes Example: Vesuvius, Mt. St. Helens, Mt. Fuji (dormat) (page s 113 red book)

Volcanoes • Types of Lava Basaltic magma—dark colored with lots of water, low in

Volcanoes • Types of Lava Basaltic magma—dark colored with lots of water, low in silica produces quiet nonexplosive eruptions. Hawaiian term: pahoehoe— very thin liquid lava forms ropelike structure when cools aa—when hardened crust of lava flow breaks into jagged chunks Silica-rich or granitic magma—light colored lava causes explosive eruptions

Volcanoes • Projectile terms: volcanic dust—smallest particle volcanic ash—rock particle size of rice grains

Volcanoes • Projectile terms: volcanic dust—smallest particle volcanic ash—rock particle size of rice grains volcanic bombs—larger rock particles a few centimeters to several meters cinders—golf ball size volcanic bombs Ring of fire—along the pacific plate approximately 300 volcanoes