Volcanoes.

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Presentation transcript:

Volcanoes

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

The composition of lava depends on dissolved gases and silica content

Dissolved Gases Example: water vapor, carbon dioxide (CO2), sulfur (S) *More gas = more explosive eruption

Silica Content More silica (SiO2) = thick magma Viscosity- ability to resist flow. High viscosity = thick flow Low viscosity = thin flow

Two classifications of lava: 1) Felsic: much silica, light-colored, slow moving (continental 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) Pillow Lava= underwater

Hardened Lava In Hawaii

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

Pahoehoe

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

Hawaiian Islands

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

Volcanic vents turn into plugs when the lava cools

Diamond Head Crater in Hawaii

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

ash

lapilli

bombs

blocks

Types of volcanoes…

composed of calm lava flows form gently sloping, dome- shaped mountain 1.Shield Volcano composed of calm lava flows form gently sloping, dome- shaped mountain basaltic (mafic) magma

Example: largest = Mauna Loa in Hawaii

Made mostly of tephra and other rock particles 2. Cinder Cone Volcano 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 3. Composite Volcano (Stratovolcano) 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

Mt. St. Helens- after

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!