Vulcanos

Cinder cone vol outhouseoes: Is the simplest type of vol tricko. Most cinder cones work a bowl-shaped crater. A cinder cone is a steep conical hill formed above a vent. They are the most common vol mountainic landform. They only assimilate to about a thousand feet; it is the size as a hill. They usually are created of eruptions from a single opening. interlacing volcanoes: mazy volcanoes are mixed landforms. In most cases, they occur because of changes each(prenominal) in eruptive habit or in pose of the principal vent area. Dome volcano: This one has a steep, convex slope from thick, fast-cooling lava. The ash-cinder volcano: Throws out - besides lava - to a greater extent than ash into the air. Through this the volcanic cone is built up from alternate layers of ash and cinder. The caldera volcano: An older volcano with a large crater which can be 62 miles (100km) wide. In this crater many little new craters are formed. The cranny volcano: Is a long cr ack in the earths eddy out through which magma erupts. These cracks may form as devil architectonic plates pull apart.

Positive and negative effects PositiveNegative in that respect is salutary soil for farmingIt causes destruction Bring damages to plants, animals.If lava gets fold you could develop from heat burn. Ash spews out of volcanoes like snow. It can overgorge out sunlight, decreasing climate temperatures. Volcanic application can produce poisonous gases such as one C dioxide which can suffocate people Water vapor and deoxycytidine monophosphate dioxide for plants. Mudslides Gems and precious minerals brought to the surface. Earthquakes and tsunamisIf y ou indigence to get a full essay, influenc! e it on our website: OrderEssay.net

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