18/08/2019
Ephemeral thermal springs
The “mungāru” monsoon, after an erratic beginning during June this year, in the Karavali and Malnad regions of Karnataka, continued unabated, further with a heavy down pour during the month of August 2019. The heavy rains mercilessly flooded our poorly planned city roads (devoid of appropriately designed storm drainages) as well as clogged river channels causing heavy havocs on innocent people living nearby the flood plains and their properties. Apart from these disasters, massive landslides and land disruptions on arterial highways, especially in Ghat sections, took their own tolls on the unsuspecting residents and travelling public.
Among the freak disasters that characterize the heavy monsoons in Western India, the occurrence of occasional ephemeral thermal springs in the Karavali coastal land deserves the attention of inquisitive geologists, environmental enthusiasts and the smart public.
Ephemeral thermal springs
On August 6, 2019, early in the morning around 6.00 AM, inmates of Appi’s house at Mundaguri colony near Caribbean resort, Chitrapu Gajani area in the outskirt of Mulki, Mangaluru Taluk had a surprise in store in the small open well located in front of their modest house. Warm fumes were emanating out of their small well lined with concrete rings. The well is located in the coastal sandy alluvium is only about 4m in depth and the static water level is slightly below the ground level. The well water which was normal and potable till yesterday night, was fuming with warm vapors and the water was perceptibly hot, about 37-38 degrees centigrade.
A team of officials including geologists from the Department of Mines & Geology visited the site in the afternoon. I was invited and went to the site along with the geologists. By the time we reached the emanation of warm fumes in the well had stopped and the degree of heat in the water was also dwindling (to about 35 to 36 degrees C).
We predicted that it is a case of leakage of geothermal energy from the reactivation of deep fractures in the area. The temperature in the well subsided and became normal the next day onward. We have encountered a similar case history earlier in an open well located near the premises of Sri Rājarājeshwari temple at Polali, Bantwal Taluk, Dakshina Kannada a few years ago.
I would like to designate this case as an incidence of ephemeral thermal spring, attributable to random release of geothermal energy due to reactivation of deeper fractures on account of the neo-tectonic plate movements on the Karavali coast. It appears that the heavy rainfall in the region and the consequent accumulation of water in the deeper fractures, enhances the pore water pressure that induces structural disturbances leading to ephemeral release of geothermal springs accompanied by vapors.
Please feel free to offer your comments or the opinion on the issue.