Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries.

Volcanoes

How do volcanoes work? Heat and pressure cause rocks to melt and form magma. Magma needs to get out, too much pressure!!!!!! Rise in temperature or drop in pressure causes magma to form faster.

How do volcanoes work? Magma is forced onto Earth’s surface. It dries and hardens, this happens many times over thousands of years. Eventually a mountain called a volcano is formed.

Parts of a Volcano Most volcanoes share a specific set of features. The magma that feeds the eruptions pools deep underground in a structure called a magma chamber. At Earth’s surface, lava is released through openings called vents. Flowing lava in the interior travels through long, pipelike structures known as lava tubes.

Where do most volcanoes occur? Volcanoes occur at both divergent and convergent boundaries and also at hot spots.

Hot Spots form volcanoes.

Prominent Hot Spots Around the World

Volcanoes form at convergent plate boundaries.

Volcanoes form at divergent boundaries.

Volcanoes at Divergent Boundaries At a divergent boundary, the lithosphere becomes thinner as two plates pull away from each other. A set of deep cracks form in an area called a rift zone. Hot mantle rock rises to fill these cracks. As the rock rises, a decrease in pressure causes hot mantle rock to melt and form magma. The magma that reaches Earth’s surface is called lava. Basaltic magma rises to Earth’s surface through these fissures and erupts nonexplosively

Why do we have different types of Volcanoes? The process of magma formation is different at each type of plate boundary. Therefore, the composition of magma differs in each tectonic setting. Tectonic settings determine the types of volcanoes that form and the types of eruptions that take place.

Viscosity Viscosity is defined as the resistance to flow. The more viscous magma is, the more explosive the eruption.

Types of volcanoes

Types of volcanoes Shield volcano: usually form at hot spots, from non explosive eruptions Cinder cone volcano: form from explosive eruptions, very steep. Composite volcano: form from both explosive and non explosive eruptions.

Shield volcano Lava has low viscosity and flows great distances as it cools. Very wide, not to steep. Biggest type of volcanoes Tallest mountain in the world is Mauna Kea (measures from sea floor to top) non explosive eruptions

Mauna Kea, Hawaii

Cedar Hill Box Elder County, Utah Note the classic shield shape of this one million year old volcano.

Cinder cone volcano Smallest type of volcano Most common Form a large crater Explosive eruption which builds up steep sides. Gas rich magma erupts explosively into air producing large fragments of solid material called cinders Lava has high viscosity Explosive!

Paricutin, Mexico

Diamond Cinder Cone, Washington County, Utah

Cinder cone volcano: Monti Silvestri, Mt. Etna- erupted 1892

Composite volcano: Eruptions alternate between explosive and non-explosive. Sometimes they have runny lava layers, other times the have pyroclastic materials form layers. Have a wide base and steep sides. Have a crater

Mount Fuji

2 Types of eruptions Explosive: volcanoes that build enough pressure to blow its top, sending pyroclastic material into the air. Non explosive: Build only enough pressure to allow lava to run down its sides.

Pyroclastic materials Material that is thrown into the air during an explosion. Volcanic bombs: large blobs of magma that harden in the air. pebble size rocks Volcanic ash: tiny powder like material

Four types of lava Aa: lava that is thick and sharp Pahoehoe: lava that forms thin crust and wrinkles Pillow lava: lava that erupts under water, has a round shape Blocky lava: cooler, lava that does not travel far from eruption, jagged when it dries.

Aa lava that is thick and sharp

Pahoehoe: lava that forms thin crust and wrinkles

Pillow lava lava that erupts under water, has a round shape

Blocky lava cooler, lava that does not travel far from eruption, jagged when it dries.