Cinder Cone Volcano Research Paper

CINDER CONE VOLCANO The cinder cone volcano, commonly found in volcanic areas, are constructed of rocks and ashes. Gas created from the lava is blown into the air which then “cools and solidifies as small rocks or cinders”. Cinder cone eruptions “take place in basaltic volcanic fields” that immensely effect the human population surrounded by it. Cinder cone eruptions majorly impact the environment by distributing volcanic gases, volcanic landslides and blasting tephra. One of the long-term impacts on human environments caused by cinder cone volcanoes are volcanic gases. During major explosive eruptions, “huge amounts of volcanic gas” and ash are injected into the stratosphere. Most are removed within “several days to weeks” but volcanic
These landslides will destroy anything presented within its path; often causing large debris-filled eruptions. These deadly streams of molten lava will often bury valleys, lakes, hills and “closed depressions”. They are extremely hazardous to human environments as they are built on size and mobility often traveling at around “100 km/hr” or more. Volcanic landslides can indirectly cause other human sufferings such as earthquakes and tsunamis – killing thousands of organisms every year. “Deposits may bury agricultural fields and villages”, causing the need for large amounts of rebuilding money. Cinder cones are well-known for their blasting of tephra, or “fragments of volcanic rock and lava regardless of size that are blasted into the air by explosions”. Tephra and volcanic ash often travel long distances from a cinder cone volcano, forming the geographical land features as well as causing destruction along the way. Volcanic activity leads to the dreaded clouds of dust that cover man-made environmental structures. “It covers just about anything” ranging from farmland to water systems. Parts may be damaged from “ash-clogged air filters” destroying most natural works and