Lonar

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    GEOLOGICAL STUDY TOUR

    AT

    LONAR LAKEAN EXCURSION REPORT

    INTRODUCTION

    Lonar lake, near Lonar village in the Buldhana District, is not just

    he source of Excitement for the visitors but also for the scientist

    community. Lonar is the third natural salt-water lake in the world, with

    a diameter of 1800 meter. It comes after Bosmatvi lake in Ghana,

    which has a diameter of 10000 meter and New Cubec lake in Canada

    with a Dai of 3500 meter.

    The lake is circular except on the north-east side, where siltation

    caused by the Dhara has created small mudflats. The diameter of the

    lake is about 1600m. The crater is 150 meters in depth and is

    absolutely confined from all sides by the walls of the crater and thereis not a single channel of water draining away from it, thereby leaving

    the lake waters stagnant for thousands of years, a large portion of the

    lake is rather shallow, preserving about 2meters of water during the

    monsoon months. This may get reduced to only a few inches during

    the summer. However, the lake is dried up completely in the year

    1991.

    HISTORIC BACKGROUND

    The official dug up the heart of the lake and conducted experiments on

    the material gathered from there, before making their announcement

    public. The scientists also found some mineral found mostly in meteor-

    hit areas. Traces of Sodium Carbonate and magnetic properties were

    also observed in the soil there. Apart form its scientific importance;

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    Lonar also occupies a place of prominence in our ancient scripts. It

    finds mention in "Aaina-E-Akbari" During the days of Emperor Akbar, a

    salt factory was located here.

    According to Sanskrit Literature, Lonar was called "Viraj Kshetra"

    in ancient times. It finds mention in "Viraj Mahatmya" a chapter in

    "Skanda Puran and Padma Puran" Sanskrit works. According to Lonar

    Mahatmya in ancient times, Kashyap Rishi had many sons. One of

    whom was believed to be staying in the vicinity of Lonar Lake. When

    Lavanasur terrorized the people and rulers of the region, the son of

    Rishi Kashyap had prayed to Lord Vishnu to kill Lavanasur. In the 13 th

    Century, a temple of Lord Vishnu as constructed there during the

    Chalukya Raj. The temple still exists and is 150mt long and 450 mt.

    wide. IT is a fine example of the quality of architecture practiced and

    perfected during that era. Near the Lonar Lake is the Paphareshwar

    pilgrimage. The engravings on the temple located there are in Sanskrit

    and sadly they have still not been deciphered.

    To add to its natural beauty the Lake has enough fauna in its

    surroundings making it a serene and scenic spot.

    ORIGIN OF LONAR LAKE

    The Lonar crater has attracted the attention of world geologists

    for investigation of its origin and the source of salinity of lake water.

    Malcamson (1840), Bradley (1853), Smith (1857), Brandford (1870),

    Medlicott and Brandford (1879), Oldham (1909), Nandi and Dev (1961),

    Venkatesh (1983), Mishra (1987) and Badve and Kumaran (1992) have

    suggested the views about the origin of the Lonar, according to them

    the crater was believed to formed by some phase of volcanic activity.But the work of Beals et al (1960), Arogyaswamy (1962), the evidence

    of glassy objects near the Lonar crater (Nayak 1972), impact affected

    minerals by Fredrickson et al (1973), Fudalay and Fredrickson (1992)

    and Haggerty and Newsom (2003) suggested that the Lonar crater was

    formed by the impact of a meteorite.

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    According to scientists, about 50,000 year back a massive

    meteor entered into the Earth's gravitational forces range. 60 meter

    long and weighing 20 lac ton it was racing at a speed of 25 km per

    second towards the planet. When it struck the earth the energy

    released was equivalent to that released by six-megaton atom bombs.

    The impact was so severe that rocks from all sides came o the surface

    and reached the height of 20 meters. The impact was so severe that it

    left a massive crater 170 meters deep and with 1800 meter in

    diameter. Today it is natural salt-water lake.

    The lake was first brought to notice in 1823 by British officer C J

    E Alexander. In 1896, American geologist G K Gilbert conducted

    studies to prove that Lonar was created due to meteor strike. An

    extensive study conducted on the spot under the leadership of Prof. K

    Fredrikson by officials of Geological Survey of India, United States

    Geological survey and other institutions, proved using Cosmic Ray-

    dating that the lake was created by a meteor hit 50,000 years ago.

    GEOLOGY OF THE AREA

    Geologically, the area belongs to Deccan Basalt formations of

    late Cretaceous to early Eocene period. The rocks observed in the lake

    are compact, vesicular and amygdaloidal basalt. At places the red bole

    beds separated the two lava flows. The basalt flows dip away from the

    depression. No appreciable fracturing or shattering is noticeable in the

    rocks. Compact basalt rocks are highly jointed and weathered around

    the joints. The compact basalt also shows the spheroidal weathering in

    the area.

    The impact of meteorite yielded the rare mineral called themuskelynite, which is transformed plagioclase feldspar. Around the rim

    of crater scattered glass splinters from 10 to 15 cm in length is

    observed. These are same like glass pieces and spherules collected by

    Apollo astronauts on the moon (India Today 15 August 1979).

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    SALINITY OF LAKE WATER

    The most striking feature of the lake is its extreme salinity and

    high alkalinity (the PH reaches the mark of 10.5 when tested with a PH

    paper). The perennial nature of the lake may be due to this high

    alkalinity, so that, as evaporation proceeds, the concentration of the

    dissolved alkaline matter is increased and, in due course, the

    evaporates begin to separate out, which gradually form a more or less

    continuous scum over the surface of water, thereby considerably

    retarding the rate of subsequent evaporation. The salinity and

    alkalinity of this continental, inland lake is attributed to the age of the

    lake and also to the mode of formation the crater.

    AMBER LAKE

    There is a small circular depression, about 700 meters away from

    the rim of Lonar crater closely resembling the main crater in its shape

    and characteristics. This is known as the Little Lonar and is believed to

    have originated from the impact of a smaller piece of the meteor,

    which split from the main body, before it hit the ground. The diameter

    of this crater is app. 340 meters and rises 6 meters above the ground

    level. This crater also has a lake, fed by three streams, which through

    the years have eroded the surrounding area causing the exposure of

    basaltic breccia. You can find pieces of rock showing typical shock

    metamorphosis caused by hypervelocity impact. Although no major

    geological research work has so far been done to establish the

    meteoritic origin of this depression, this evidences supports such a

    thesis and should be considered as an integral part of the precincts of

    Lonar crater. In 1973, Fredriksson suggested that Amber lake crater

    was formed by a fragment ejected from Lonar crater, whereas S.

    Master who surveyed the Amber crater in 1999 concluded that it was

    not a secondary crater, but was formed at the same time as the Lonar

    crater

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    GEOLOGICAL STUDY TOUR REPORT

    Submitted to

    Department of Geology

    Dnyanopasak College

    Parbhani - 431 401

    As per

    Syllabus of

    Swami Ramanand Teerth

    Marathwada University, Nanded

    Submitted by

    B. Sc. III Year

    GEOLOGY

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    For the year

    2004-2005

    CERTIFICATE

    This is to certify that Mr./Miss ____________

    _____________________________________________ of B.Sc. III year

    (Geology) has attended the geological study tour organised by

    Department of Geology, Dnyanopasak College, Parbhani at

    Lonar Lake in Buldhana district.

    This report covers the geological aspects as per the

    B.Sc. standards of syllabus of Swami Ramanand Teerth

    Marathwada University, Nanded.

    Tour Incharge Head of Deptt. External Examiner

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