Thick, sticky, high-silica magma are so viscous that they don't erupt, causing internal pressure within a volcano to rise. Earth's crust fails under high pressure, explosion eruption.
Runny, low silica, high temperature basaltic lava are so low in viscosity that they erupt quite easily and produce quiet eruptions of freely flowing lava.
No, not all volcanoes have the same characteristics. Volcanoes can vary in size, shape, eruption style, composition of erupted materials, and frequency of eruptions. Some volcanoes are steep-sided and explosive, while others are gently sloping and effusive.
There are four main types of volcanoes: shield volcanoes, cinder cone volcanoes, stratovolcanoes (composite volcanoes), and calderas. Each type has distinct characteristics based on their eruption style, shape, and composition.
There are three main shapes of volcanoes: shield volcanoes, cinder cone volcanoes, and stratovolcanoes. Each type has distinct characteristics based on its eruption style, lava composition, and shape.
Mountains, hills, and volcanoes are all types of landforms that rise prominently above the surrounding terrain. Collectively, they can be referred to as "topographical features" or "elevated landforms." Each type has distinct characteristics: mountains are generally steeper and higher, hills are lower and more gently sloping, while volcanoes are formed by volcanic activity and can vary widely in shape and size.
The main types of volcano formations are shield volcanoes, stratovolcanoes (composite volcanoes), cinder cone volcanoes, and calderas. Each type has distinct characteristics based on their eruption style and the type of materials they release.
No, not all volcanoes have the same characteristics. Volcanoes can vary in size, shape, eruption style, composition of erupted materials, and frequency of eruptions. Some volcanoes are steep-sided and explosive, while others are gently sloping and effusive.
what are characteristics of inactive volcano
There are four main types of volcanoes: shield volcanoes, cinder cone volcanoes, stratovolcanoes (composite volcanoes), and calderas. Each type has distinct characteristics based on their eruption style, shape, and composition.
Basaltic, runny magma.
There are three main shapes of volcanoes: shield volcanoes, cinder cone volcanoes, and stratovolcanoes. Each type has distinct characteristics based on its eruption style, lava composition, and shape.
The main types of volcano formations are shield volcanoes, stratovolcanoes (composite volcanoes), cinder cone volcanoes, and calderas. Each type has distinct characteristics based on their eruption style and the type of materials they release.
There are four basic types of volcanos. They are cinder cones, shield volcanoes, composite volcanoes, and lava domes. Composite volcanoes share some characteristics of all the others.
Volcanoes differ in terms of their eruption style, which can vary from explosive eruptions with ash clouds and pyroclastic flows to effusive eruptions with lava flows. They also differ in shape and size, ranging from stratovolcanoes with steep slopes to shield volcanoes with gentle slopes. Additionally, the type of magma they erupt, such as basaltic, andesitic, or rhyolitic, can vary among volcanoes.
It is difficult to determine the weakest volcano in the world as each volcano has its own unique characteristics. Volcanic activity can vary greatly, with some volcanoes being dormant for centuries while others are active more frequently. Some smaller or less known volcanoes may be considered weaker compared to more well-known and active ones.
On average, around 50-70 volcanoes erupt each year. However, the number can vary from year to year.
The time it takes to climb a volcano can vary depending on factors like the size of the volcano, its elevation, and the individual's fitness level. Climbing smaller volcanoes may take a few hours, while larger and more challenging volcanoes could take a full day or even multiple days to summit.
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