Magma liquid molten rock underground Lava magma that

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Magma: liquid, molten rock underground Lava: magma that reaches the surface

Magma: liquid, molten rock underground Lava: magma that reaches the surface

The composition of lava depends on dissolved gases and silica content

The composition of lava depends on dissolved gases and silica content

Dissolved Gases Example: water vapor, carbon dioxide (CO 2), sulfur (S) *More gas =

Dissolved Gases Example: water vapor, carbon dioxide (CO 2), sulfur (S) *More gas = more explosive eruption

Silica Content More silica (Si. O 2) = thick magma Viscosity- ability to resist

Silica Content More silica (Si. O 2) = thick magma Viscosity- ability to resist flow. High viscosity = thick flow Low viscosity = thin flow

Two classifications of lava: 1) Felsic: much silica, lightcolored, slow moving (continental crust)

Two classifications of lava: 1) Felsic: much silica, lightcolored, slow moving (continental crust)

2) Mafic: low silica and gas, dark-colored, fast moving (oceanic crust)

2) Mafic: low silica and gas, dark-colored, fast moving (oceanic crust)

3 types of mafic lava: 1) Aa Lava= choppy 2) Pahoehoe = ropy

3 types of mafic lava: 1) Aa Lava= choppy 2) Pahoehoe = ropy

3) Pillow Lava= underwater

3) Pillow Lava= underwater

Hardened Lava In Hawaii

Hardened Lava In Hawaii

Volcano: place where magma reaches the surface Volcanism: when a fissure or crack develops

Volcano: place where magma reaches the surface Volcanism: when a fissure or crack develops in the crust allowing magma to reach the surface

Pahoehoe

Pahoehoe

HOT SPOTS: areas of volcanic activity in the middle of lithospheric plates

HOT SPOTS: areas of volcanic activity in the middle of lithospheric plates

Hawaiian Islands

Hawaiian Islands

 • Volcano Anatomy 1. Vent: opening from which lava flows 2. Crater: funnel-shaped

• Volcano Anatomy 1. Vent: opening from which lava flows 2. Crater: funnel-shaped pit or depression at top of volcano 3. Caldera: depression where the walls have collapsed

Volcanic vents turn into plugs when the lava cools

Volcanic vents turn into plugs when the lava cools

Diamond Head Crater in Hawaii

Diamond Head Crater in Hawaii

Pyroclastic Material (tephra): solid particles produced in eruptions 1. Ash (<2 mm) 2. Lapilli

Pyroclastic Material (tephra): solid particles produced in eruptions 1. Ash (<2 mm) 2. Lapilli (<64 mm) 3. Bombs 4. Blocks

ash

ash

lapilli

lapilli

bombs

bombs

blocks

blocks

Types of volcanoes…

Types of volcanoes…

 • composed of calm lava flows • form gently sloping, domeshaped mountain •

• composed of calm lava flows • form gently sloping, domeshaped mountain • basaltic (mafic) magma

Example: largest = Mauna Loa in Hawaii

Example: largest = Mauna Loa in Hawaii

 • Made mostly of tephra and other rock particles • Formed from explosive

• Made mostly of tephra and other rock particles • Formed from explosive eruptions • small, narrow base & steep sides • Grantic (felsic) magma

 • Symmetrical build up of alternating layers of rock and lava • highly

• Symmetrical build up of alternating layers of rock and lava • highly explosive eruptions with high silica and high gas content • forms large, cone-shaped mountains

Composite example 1 Mt. St. Helens- before

Composite example 1 Mt. St. Helens- before

Mt. St. Helens- after

Mt. St. Helens- after

Ex. 2 -Mount Vesuvius - Pompeii 20 feet of volcanic ash smothered The city!

Ex. 2 -Mount Vesuvius - Pompeii 20 feet of volcanic ash smothered The city!

Mount Vesuvius – Pompeii= composite 20 feet of volcanic ash smothered The city!

Mount Vesuvius – Pompeii= composite 20 feet of volcanic ash smothered The city!