Types of volcanoes present on earth essay

The speed of a lava flow depends on its viscosity which depends on temperature and composition as well as the slope of the surface on which it is flowing. Dense black clouds of ashes shot 20 to 50 miles high, and were brought down as mud by the torrential rain which fell over the adjacent islands.

The Bushveld lopoliths of Transvaal, South Africa are good examples. Lassen Peak in California is an example of a volcano formed from felsic lava and is actually a large lava dome. It may appear to be a crack or fissure on the surface of the earth. It is being used for domestic heating in Italy, New Zealand and Iceland.

They may unleash ravaging rockslides and mudflows. Nuovo, near Naples and Mt. Volcanoes are said to be active when they frequently erupt or at least when they have erupted within recent time.

Spectacular sun set, extended period of darkness and stratospheric ozone depletion are all other effects of eruptions. Continued subsidence caused them to drop below the water surface. It may appear to be a crack or fissure on the surface of the earth. Later studies have revealed that most of the water is from surface precipitation, with not more than 5 per cent from the cooling magma.

If the magma contains little of either of these, it is more liquid and it flows freely forming a shallow rounded hill. Volcanoes and Atmospheric Pollution: It is made from several different layers of solidified and cooled lava, pumice, volcanic ash and tephra.

There may exist a special problem in studying the gases, both in collecting them under hazardous conditions or impossible conditions. A noteworthy type of volcano is part of the world encircling mid-ocean ridge MOR visible in Iceland. The magma accumulates at the top, one over the other and the around.

The lava flows are so viscous that they solidify after a short distance. Subglacial volcanoes These are the types of volcanoes, which are formed beneath the ice caps.

Essay on Volcanoes | Geology

There are also secondary and tertiary hazards connected with volcanic eruptions. These bubbles or voids which were filled by gas may get elongated to tube like forms during the forward movement of the viscous lava.

The less fluid lavas that explode more violently form ash and cinder cones with large central craters and steep slopes. Explosion Index for selected volcanic regions by Rittmann are shown in the table below.

Plateau Basalts or Lava Plains: Krakatau in August The fluid basic lava, flowing for long distances produces extensive lava plains and basalt plateaux, such as the great lava plains of the Snake Basin, U.

Phenomena Associated with Volcanism: Image adapted from cotf. Later as the pressure of gas and magma rises, another eruption occurs shattering the dome. After reading this essay you will learn about: Thus if a well is drilled at a place where the average surface temperature is say These features range from towering peaks and huge lava sheets to small and low craters.

The water rises to the surface without any explosion. The MOR is really a single, extremely long, active, linear volcano, connecting all spreading plate boundaries through all oceans. A classification of volcanic activity based on the type of product is shown in Fig.

A few continue into Asia Minor Mt. Its volcanic cloud lowered global temperatures by as much as 3. Fissure eruptions represent the simplest form of extrusion in which lavas issue quietly from linear cracks in the ground.

The gases and vapour increase the mobility and explosiveness of the lavas which are emitted through the orifice or vent of a volcano during a volcanic eruption.Essay on the Origin of Volcanoes Essay on the Types of Volcanoes Essay on the Landforms Associated with Vulcanic Activities Essay on the Volcanic Eruptions Essay on the Distribution of Volcanoes The ancient Greeks believed that volcanic eruptions occurred when Vulcan, the God of the Underworld.

Types of Volcanoes Present on Earth Volcanoes get their name from the Greek word Vulcano. "To the ancient Greeks, Vulcano was Hiera Hephaistou to the ancient Romans it was the home of the forges of Vulcan; to both Vulcano was the lair of the god of fire" (Bullard ).

Volcanoes generally erode away, they are not often preserved in the geologic record, but we can infer what types of volcanoes were present by the volcanic deposits left behind.

The large, violent volcanoes, called stratovolcanoes, often produce pyroclastic flows. Flows of water and ash and tephra, called lahars, flow rapidly down the steep-sided stratovolcanoes and form thick deposits. Essay # 1.

Analysis of Volcanoes

Introduction to Volcanoes. A volcano is a cone shaped hill or mountain which is built-up around an opening in the earth’s surface through which hot gases, rock fragments and lavas are ejected.

Stratovolcanoes consist of many layers (strata) of hardened lava, tephra, pumice, and volcanic ash. They generally have steep slopes and are the most common type of volcanoes on Earth.

Volcanoes can be one of the most destructive forces on Earth.

The Three Main Types of Volcanoes

It is estimated that some million people live near active volcanoes (Lutgens and Tarbuck, ). Of the Earth's known volcanoes, 70 can be expected to erupt each year with at least one large eruption each decade (Lutgens & Tarbuck, ).

Types of volcanoes present on earth essay
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