Stratovolcanoes are often called composite volcanoes, the type that most people recognise as volcanoes. With peaks reaching several hundred metres in height from their surroundings, they dominate the visual landscape of the area. is composed of a mixture of pyroclastic deposits and lava flows. Indirectly, a stratovolcano is formed from multiple layers of viscous lava flows and other eruptive materials. Most stratovolcanoes have a complex structural form caused by repeated eruptions. Some of these types of volcanoes form over several thousand years, but may become active again tens or even hundreds of years later and rest again during the same time frame. This is due to the eruption of andesite rocks. The slope of the stratovolcano type is usually between 30-50 degrees and the eruption comes from continuous activity in the stomach which is then pushed out to the earth’s surface (ESDM, 2022).