Despite the many negative effects associated with the volcanoes, there are some groups that find living near them very beneficial. It turns out that volcanoes have a lot to offer to these groups, as long as they are ready to beat it once a notice is issued. For many, who stare from a distance while the eruptions occur could wonder why would someone opt to live under such hazard conditions. According to Kelman, & Mather, (2008 ), there are various reasons as to why people find living near volcanoes beneficial, among them being that the soils are very fertile for farming, these places are centers for tourists' attractions, for some cultural practices, and energy provision. It, therefore, goes with no say that the particular demographic population that stays here know its benefits.
Every farmer who is a good practitioner in his work knows very well how rich the soils around volcanoes are. However, the rocks have to decompose over years for them to make rich soils for crop growing. An example of such an area is the slopes of Vesuvius in Italy. Moreover, the locals living around these areas are employed as tour guides, as millions of tourists come to see the fascinating scenes of erupting and erupted mountains, bathing lakes, hot springs, and geysers. Many businesses flourish here, such as restaurants and hotels and gift shops.
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For cultural callings, most of the groups find it hard to relocate and abandon their ancestral lands. For example, the Hawaii natives relate volcanoes to gods who their ancestors worshipped. More to this, there is a big population that lives here to benefit from the geothermal power generated in this area. With most of the people working in these geothermal stations, while others use the readily available power to run their small industries located at these places. Countries such as New Zealand highly depend on volcanoes for its electricity.
References
Kelman, I., & Mather, T. A. (2008). Living with volcanoes: the sustainable livelihoods approach for volcano-related opportunities. Journal of Volcanology and Geothermal Research , 172 (3-4), 189-198. https://doi.org/10.1016/j.jvolgeores.2007.12.007
