Vulcanos

Cinder cone vol outhouseoes: Is the simplest type of vol tricko. Most cinder cones urine a bowl-shaped crater. A cinder cone is a steep conical hill formed above a vent. They are the most common vol tail endic landform. They only receive to about a thousand feet; it is the size as a hill. They usually are created of eruptions from a single opening. interlacing volcanoes: manifold volcanoes are mixed landforms. In most cases, they occur because of changes apiece in eruptive habit or in compel 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 - more 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 fling volcano: Is a long crack in the earths c hange form out through which magma erupts. These cracks may form as both architectonic plates pull apart.

Positive and negative effects PositiveNegative in that location is salutary soil for farmingIt causes destruction Bring damages to plants, animals.If lava gets stuffy you could develop from heat burn. Ash spews out of volcanoes like snow. It can overgorge out sunlight, decreasing climate temperatures. Volcanic action mechanism can produce poisonous gases such as degree centigrade dioxide which can suffocate people Water vapor and carbon copy dioxide for plants. Mudslides Gems and precious minerals brought to the surface. Earthquakes and tsunamisIf you indigen ce to get a full essay, enjoin it on our we! bsite: OrderEssay.net

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