Hot springs can form in several ways, but most commonly occur when rainwater or groundwater is heated by magma underneath Earth's surface. Cracks or faults in the Earth's surface allow water to flow deeper towards the mantle, where it comes in contact with hot rocks that heat the water. Underground pressure then forces the hot water upwards, back to the Earth's surface through the same cracks or faults. The amount of underground pressure determines how fast and how far the hot water flows. This type of hot spring usually forms in areas with volcanic activity.
Hot springs can also be formed when absorbed rainwater is heated underground by the radioactive decay of elements present in the rock. For every 1,000 feet of depth, the groundwater is heated by an additional 15 °F. Additionally, the hot water becomes more viscous and rises up through cracks and faults to the Earth’s surface. As the hot water reaches the surface, it can flow slowly or quickly depending on the amount of underground pressure. Generally, the flow rate of hot springs differs depending on the volume of underground water and the amount of underground pressure.
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Answer: Yes we have a hot spring in our area Its Called Mambukal Hot spring, No there is no presence of Volcano in my area
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Hot springs can form in several ways, but most commonly occur when rainwater or groundwater is heated by magma underneath Earth's surface. Cracks or faults in the Earth's surface allow water to flow deeper towards the mantle, where it comes in contact with hot rocks that heat the water. Underground pressure then forces the hot water upwards, back to the Earth's surface through the same cracks or faults. The amount of underground pressure determines how fast and how far the hot water flows. This type of hot spring usually forms in areas with volcanic activity.
Hot springs can also be formed when absorbed rainwater is heated underground by the radioactive decay of elements present in the rock. For every 1,000 feet of depth, the groundwater is heated by an additional 15 °F. Additionally, the hot water becomes more viscous and rises up through cracks and faults to the Earth’s surface. As the hot water reaches the surface, it can flow slowly or quickly depending on the amount of underground pressure. Generally, the flow rate of hot springs differs depending on the volume of underground water and the amount of underground pressure.