Tremors in Jawhar scare villagers -minor tremors between 1983 and 1996.Tremors in Jawhar scare villagers Ram Parmar email@example.com
Fresh tremors were again felt in Jawhar on Monday morning.Since August 26,villages in the tribal belt have been experiencing tremors.Scientists from the India Meteorological Department (IMD),Colaba,and National Disaster Response Force (NDRF),Pune were to arrive in Jawhar late Monday evening.The Thane District Disaster Management Squad are pacifying the terrified tribals and holding public awareness meetings.
Nitin Naik,Chief,District Disaster Management Squad,Thane,said his team is in Jawhar after Tehsildar Urmila Patil informed him about fresh shocks on Monday morning.Three tremors were recorded since 9.00 am,said Naik.
Some of the utensils fell from the racks and our huts also shook, said Harshad Patil,a resident of Kalidhond.
We panicked and ran out of our homes and stood in the open, said Mohammed Hussain,another resident of the same village.
We are quite surprised with these shocks as even the seismic apparatus kept at the IMD,Colaba has not recorded them.But we are not taking any chances and have informed the IMD and the NDRF,and scientists are to arrive in Jawhar by late Monday.Only after they analyse the situation,we can arrive at a conclusion, said Naik.
When asked whether the incident could be due to stone quarrying in the jungle areas of Jawhar,Naik said the government has banned quarrying and other activities during the monsoons.The shocks could be due to the massive explosive activities being carried out by the Irrigation department,Thane to lay underground water pipelines.The pipes are being laid around 800 m underground.But this is an assumption, said Naik.
The Seismic Environment of Mumbai
There have been claims that Mumbai is prone to moderate intensity earthquakes ranging up to about 6.5 on the Richter scale.
Mumbai lies over more than 10 seismic fault lines (black lines in the map). Major fault lines lie along the Thane creek, Ulhas river, the Manori and Malad creeks and the lakes. To the west, a fault line stretches from Colaba to Vasai, touching Malabar hill.
A major junction of three faults, the Thane, Panvel and Dharamtar creeks lies close to the Oil and Natural Gas Commission's oil plant in Uran in New Mumbai.
The coastal plain to the east of Mumbai is prone to earthquakes of even higher intensity, upto 7.5 on the Richter scale. In this region the black volcanic rocks of the Western Ghats have been eroded by the action of the sea. The resulting relief of pressure on the underlying rocks has created many fault lines along the coast.
FEW YEARS AGO THERE WAS A SIMILAR EARTH QUAKE; IN JAWAHAR; WHICH WAS FELT ALLOVER MUMBAI .
THE CONCERNED GOVERNMENT DEPARTMENT MUST MAKE DEEPER STUDIES ABOUT THIS ;INSTEAD OF SAYING THAT IT MAY BE BECAUSE OF PIPE LINE ETC
Jawhar recording minor tremors between 1983 and 1996.
Letter to Editor
Movers and shakers
June 2005 has turned out to be an unusual month for the northern city of Kalyan, situated on the bank of Ulhas river, with two minor earthquake tremors, both of magnitude 3.0, shaking it and neighbouring Ambernath and Dombivli, on the evening of June 14 and again on the morning of June 18.
Though they did not cause any damage, they show that the eastern corridor beyond the Thane Creek is seismically quite active and this is significant.
Such low earthquake activity persisted in the northern part of Thane district earlier too, with Khardi, Bhatsa, and Jawhar recording minor tremors between 1983 and 1996. But, after 1998, the earthquake activity shifted southwards to the tract falling between Kalyan and Panvel except for one stray occurrence near Palghar in December, 2001.
Two of the most recent tremors May 31, 1998 of magnitude 3.6 and the other that occurred on November 16, 2001 of magnitude 3.0 were epicentred at Ambhe village, 10 km east of Taloja and Khairna, 10 km west of Taloja, close to the Thane Creek. Both shocks that occurred in June, 2005 were epicentred at Kalyan.
Why Kalyan rocks
The main reason for persistent seismic activity, even if it is of low magnitude, at the corners of a triangle connecting Kalyan, Khairna and Ambhe, is the major geological transition that has taken place in this terrain to the west of Kalyan in the north and Panvel in the south.
The rock in this region is a black basalt of volcanic origin, having been poured out of long and deep fissures in a hot, molten state in the geological past. This basalt rock occupies a staggering 5,00,000 sq km of Deccan Volcanic Province that covers major parts of Madhya Pradesh, Maharashtra and Gujarat.
The most important aspect is that this basalt lies in a perfectly horizontal position at all places located to the east of the Kalyan-Panvel line as seen clearly in the hill forms flat-topped plateaus and ridges like the ones at Khandala and Mahabaleshwar.
But immediately to the west of this line the geological scenario changes drastically and the same black rock occurs here with a distinct slant, called dip, in a westerly direction as observed in the hills around the Powai Lake.
Tension in Panvel too
Such a geological feature that imparts a tilt to horizontally laid rocks is called a monoclinal flexure and Dr J B Auden, a British geologist who was the first to recognise this feature in this region, christened it the Panvel Flexure since it starts from Panvel at its southern end and runs northward through Kalyan and turns northwest.
This important Panvel Flexure owes its origin to a tensional stretching of the rocks in a westerly direction.
It is well known that tension always leads to rupture and such a tensional pull of the rocks had consequently led to the formation of many geological faults (which are in fact rupture planes over which the rocks on either side have moved past each other) in the region; these faults had weakened the rocks of the terrain considerably and made them vulnerable to earthquakes.
Cost of staying safe
Important townships like Navi Mumbai, Belapur, Mumbra, Ambernath, Dombivli and Badlapur besides Kalyan are located in this active seismic belt.
Given that earthquakes can neither be predicted nor prevented, precautions are necessary. Following standard building codes for different civil engineering structures during construction is the only precaution.
Earthquake-resistant designs which include an additional safety factor in view of the seismic risk, are available for all types of buildings and these increase overall cost of construction only by about 10% which is well worth providing for.
How high can you go?
Buildings with 40-50 floors are problematic and may be avoided.
Seismologists are not able to ensure safety beyond a certain optimum height; a state-level committee had recommended restricting heights to 70 metres (about 22 floors) and this seems reasonable.
It is argued that high-rises can be built on raft foundations which will make them float like ships during earthquakes but recent research at Pennsylvania State University has shown that high-rises may not always come back to their original vertical positions after the earthquake vibrations pass off but, instead, remain tilted.
Likewise, existing buildings should also be reinforced to withstand earthquake vibrations.
California is preparing itself
Complacency should give way to caution considering the seismicity of the Kalyan-Panvel corridor.
It will be good to increase the level of awareness about earthquake possibilities and get into a mood of preparedness as the Americans are doing in California which is a highly seismic state; their calculations lead them to believe that a major earthquake is due on the San Andreas Fault in the San Francisco area sometime between 2010 and 2030 and they are already gearing themselves towards that possibility after nearly a century their last major earthquake occurred in 1906 at San Francisco.
As for Mumbai
Mumbai seems to be somewhat favourably located to the west of the Thane Creek in a terrain with fewer faults and so earthquakes have so far avoided the commercial capital of India. However, it still figures in Seismic Zone 3 and therefore can draw its lessons from the Kalyan tremors.
An earthquake of magnitude 6.5 occurring anywhere in the Kalyan-Panvel corridor will affect all the places in the Mumbai Island. One can only hope that the Thane Creek will continue to act like the Lakshman Rekha and hold the earthquakes at bay!
The writer is an ex-Professor of Geology, IIT Bombay at Powai and an earthquake geologist
Some of the important faults occurring in this region are: the Thane Creek Fault, the Panvel Creek Fault and the Ulhas River Faults.
These faults are responsible for the minor earthquakes in this eastern corridor by getting reactivated periodically. It will be seen that the Ulhas River west of Kalyan flows along many small unusual meandering loops all of which would appear to be faulted segments.
These tiny faults and the major fault along the Panvel Flexure itself surround Kalyan closely and make it a potential venue for earthquakes.
Likewise, the Thane Creek Fault (which is an established feature by now) had given rise to the Khairna tremor of 16-11-2001 while the Panvel Creek Fault had obviously triggered the Ambhe earthquake of 31-5-1998.
It needs to be noted that this major geological transition zone lying to the east of Thane Creek is a highly faulted tract and this makes it vulnerable to earthquakes.