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Posted on April 14, 2022 (Updated on July 9, 2025)

What kind of lava does pahoehoe form?

Regional Specifics

basaltMafic (ferromagnesian, dark-coloured) lavas such as basalt characteristically form flows known by the Hawaiian names pahoehoe and aa (or a’a). Pahoehoe lava flows are characterized by smooth, gently undulating, or broadly hummocky surfaces.

What is pahoehoe aa and pillow lava?

Lavas, particularly basaltic ones, come in two primary types: pahoehoe (pronounced ‘paw-hoey-hoey”) and aa (pronounced “ah-ah”). Both names, like a number of volcanological terms, are of Hawaiian origin. A third type, pillow lava, forms during submarine eruptions.

What is a pillow of lava?

Pillow lavas are bulbous, spherical, or tubular lobes of lava. They form during eruptions with relatively low effusion rates. Slow extrusion gives enough time for a thick crust to form on all sides of a pillow lobe, and prevents individual pillows from coalescing into a sheet.

What is pahoehoe lava?

“Pahoehoe” is a Hawaiian word used to describe a lava flow with a smooth, ropy surface. Pahoehoe flows advance slowly, with small amounts of lava squeezing out of a cooler crust. Pahoehoe flows can exhibit all kinds of different shapes as they form and cool. These are sometimes called “lava sculpture.”

What are the three main types of lava and how are they different?

The high temperatures and pressure under Earth’s crust keep magma in its fluid state. There are three basic types of magma: basaltic, andesitic, and rhyolitic, each of which has a different mineral composition. All types of magma have a significant percentage of silicon dioxide.

What are the differences between pahoehoe and aa what kind of eruption produces these types of lava?

Pahoehoe has a smooth wavy surface that resembles twisted rope. It advances by extruding molten toes of lava beneath a thin, flexible crust. As it travels pahoehoe lava often changes to blocky flows called aa. The surface of aa lava is brittle and rough, covered in broken lava blocks called clinkers.

Which is faster pahoehoe or aa?

AA lava moves fast whereas Pahoehoe moves slowly. In the case of AA lava flow, gases have escaped from the upper surface creating clinkers and jagged outer structure.

Why is pahoehoe lava smooth?

The low velocity of pahoehoe flows means that the skin that forms by air-cooling is not disrupted during flow and can maintain its smooth, unbroken, well-insulating surface. Thus the temperature and viscosity of lava do not change very much even tens of kilometers from the vent.

Is pahoehoe lava mafic or felsic?

Mafic lava, which forms much of the oceanic crust, is high in magnesium and iron. Mafic lava is primarily responsible for forming the Hawaiian Islands. Two common forms of mafic lava flow are known by their Hawaiian names: pahoehoe and aa. Pahoehoe lava is billowy lava that is often wrinkled and ropy in appearance.

How do craters differ from Calderas?

What is the difference between a crater and a caldera? A crater is a funnel shaped pit at the top of a volcanic vent whereas a caldera is a basin shaped depression formed when the volcanic cone collapses due to magma chamber below getting empty of magma.

What is the principal difference between craters and calderas quizlet?

Composite cones are created by a mixture of explosive activity and lava flows. What is the principal difference between craters and calderas? Calderas are much larger depressions created by collapse of the upper portions of the volcano. You just studied 20 terms!

Are calderas bigger than craters?

Craters are typically smaller than calderas, and are often bowl-shaped. Calderas are larger, and typically have a more circular shape. The principal difference between craters and calderas is their size: calderas are much larger than craters.

What is one way that cinder cones differ from composite and shield volcanoes?

What is one way that cinder cones differ from composite and shield volcanoes? Cinder cones are smaller than composite and shield volcanoes.

Why do lava domes and composite volcanoes differ in morphology?

Unlike composite and shield volcanoes, lava domes are of significantly smaller stature. They are formed when the lava is too viscous to flow to a great distance. As the lava dome slowly grows, the outer surface cools and hardens as the lava continues to pile within.

When contrasting lava from a composite volcano to lava from a shield volcano?

When contrasting lava from composite volcanoes to lava from shield volcanoes, composite volcanoes most often produce silica-rich lavas with high viscosities, whereas shield volcanoes produce basaltic lavas with low viscosities.

What is the difference between aa lava and pahoehoe lava quizlet?

Pahoehoe is lava that in solidified form is characterized by a smooth, billowy, or ropy surface, while aa is lava that has a rough, jagged, spiny, and generally clinkery surface.

What volcanoes have pahoehoe lava?

Kilauea volcano, Pu’u O’o vent. Forming basaltic pahoehoe lava flow in Hawaii. Such lava flows move slowly and are not overly dangerous when compared with some other volcanic phenomena.

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