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Anatomy of a Volcano—Tertiary Features
Produced by the collapse of a volcano into its emptied magma chamber
1. Lava • Molten rock released
during a volcanic eruption.
• Can be mafic (thin, and very fluid), felsic (thick and chunky), or intermediate (a mix of mafic and felsic)
2. Gases • Form from the mixture of ground water with magma and solid rock below the surface– often acidic
3. Pyroclastics (Tephra)• Solid rock produced during an eruption• Sources – neck, cone, lava cooled in the
atmosphere Size
ash—small (looks like
smoke) blocks—angular
up to 6 meters bombs-rounded
up to 6 meters
1. Shield Volcanoes
• Form from oceanic crust; mafic lava
• Slope of cone is <5o
• Example: Hawaii• Eruption: mostly
lava; have few gases or pyroclastics; eruptions can last for months or years
2. Composite (or Strato) Volcano• Form on continental
margins with intermediate lava
• Moderate slope 15-30o is typical
• Example: Mt. St. Helens, Washington
• Eruptions– a mixture of lava, gases, and pyroclastics; a delay of 50-350 years is possible between eruptions
3. Cinder Volcanoes• Form from continental
crust; felsic• Steep slope >30o
• Example: Crater Lake, Oregon
• Eruptions: mostly gases and pyroclastics; very little lava (if any); very violent eruptions (often destroy the cone)