Eternal India
encyclopedia
ARCHAEOLOGY
building obstructing the view of the famous temple of Dwar-
akadhish at Dwaraka noted for Krishna worship was demolished
and to everyone’s surprise a beautiful temple of Vishnu assignable
to 9th century A.D. was uncovered. Its roof was damaged by the
sea, but the walls, and plinth were preserved by the sand deposit.
This discovery acted as an incentive to dig deeper anti trace earlier
remains of temples and townships if any. Further excavation
brought to light the remains of two more temples. The lower one
was datable to 1st century B.C. and the upper one to 2nd-4th
century A.D. on the basis of ceramic and numismatic evidence,
especially the coins known as
Karshapanas.
Further digging up to
10m depth exposed debris of a protohisotric settlement in which a
distinct pottery known as the Lustrous Red Ware was also found.
Similar pottery occurring in Prabhasa (Somnath), another Ma-
habharata site on the southern coast of Saurashtra, has been as-
signed to the 15th-12th century B.C. The wave-rolled pottery
found in the lowest level of the trench at Dwaraka suggested that
the proto-historic settlement here was destroyed by the sea. This
unambiguous archaeological evidence on shore increased the pos-
sibility of finding the remains of the submerged city of Dwaraka of
the
Mahabharata
period in the sea. The oceanographers were also
keen to ascertain the cause of submergence of the city. If it was
due to a rise in sea level the rate of rise could be determined more
accurately on the basis of
in situ
archaeological finds. Thus began
the search for the lost city of Dwaraka. The Department of Science
and Technology, and the National Institute of Oceanography came
forward to support a project for marine archaeological investiga-
tions in Dwaraka and elsewhere. The National Institute of Ocean-
ography (NIO) Goa, has been providing the logistic support. The
Archaeological Survey of India has been extending financial assis-
tance at times.
Before the Marine Archaeologist ventures to search for sub-
merged cities he must study the bathymetry, geology and topogra-
phy of the zone. The NIO scientists have noted a low stand of the
sea in the Gulf of Kutch 10,000 years ago. The Marine Archaeo-
logical Centre (MAC) in NIO under the direction of S.R. Rao
started exploring the Bet Dwaraka island in the Gulf of Kutch
because
Harivamsa
and other texts say that Dwaraka was a
Varidurga
‘fortress in water’. It is said to have been built in the sea
‘
Udadhimadhyastham
. In the first instance the surf zone of Bet
Dwaraka was excavated and simultaneously the Arabian Sea off
Dwaraka was also explored from 1982 through 1991. At both the
places ancient structures submerged by the sea have been found.
Modern Underwater Search Technique
Swimline technique had to be adopted-by the diver-archaeolo-
gists of MAC for surveying manually an area of 1.5 X 0.5 km
seaward of the temple of Sea God (Samudranarayana) at Dwar-
aka, and the operation was limited to 15 m depth. In 1989 the side
scan sonar, profiler, echo sounder and magneto meter surveys sup-
plemented manual and optical surveys for locating the structures
and studying the bathymetry. Photographs were taken with
Nikonos V underwater camera and video films have been produced
by deploying OSPREY underwater T.V. camera. In Bet Dwaraka
the visibility is very poor, but slightly better in the Arabian Sea off
Dwaraka. Initially fishing trawlers were engaged. From 1987
onward well-equipped modern research vessels
Vedhavati
and
Sea Master
were chartered. Ex-navy divers were trained in under-
water photography and excavation and subsequently Srinivas
Bandodkar, an expert diver-photographer, trained five qualified
archaeologists namely Dr. K. Rajan, Mr P. Gudigar, Mr. Sundaresh,
Mr. Sila Tripati, Mr. A.S. Gaur and Mr. Alok Tripathi in underwater
exploration and photography. Mr. Y.D. Sharma, Mr. U.S. Shirsat
and Mr. Sheikh Ali photographers, received training in diving and
underwater photography. The MAC is now equipped for full
fledged underwater excavation and retrieval of objects.
Geophysical Survey
The latest target search techniques involving the use of the
Echo Sounder, Mud penetrator or Sub-bottom profiler and side
scan sonar for identifying shipwrecks and submerged structures
have been adopted by the MAC. The position-fixing of the struc-
tures is done with the help of the electronic system namely Motor-
ola Miniranger III and from 1990 onwards the Global Position
Fixing System (GPS) is used. The Mini Ranger works in C band on
a line of sight principle. The mobile station installed temporarily in
the Research Vessel transmits microwave signals and the base
stations in Dwarakadhish Temple and the lighthouses at Dwaraka
and Kacchigadh receive these signals and retransmit them. These
signals are in turn received by the station (Mini Ranger) on board
the vessel. The time elapsed is converted by the Range Console
into distances that are displayed. The position of the ship thus
determined is noted as position of the buoy marking the structure or
any other archaeological object lying on sea bed. The GPS gives
more accurate location using satellite data.
For obtaining a plan view of the seabed, geological features and
anomalies which may be man-made features, the side scan sonar is
used The system is based on the back scattering property of the
sea bed. The towed transducers on either side located in the
“fish” (fig:38) enclosure transmit and receive sonar signals to and
from the seabed. As the transducer moves forward through the
water along with the vessel successive strips produce a map of the
seabed on either side of the recorded track of the sonar. Because of
the angle of the sonar that strikes the objects on the sea bed there
will be delay beyond the object before the sound strikes the seabed.
This produces a white shadow behind the strong signal allowing the
height of the object to be calculated. Sub-bottom profiler is useful
in detecting objects and sites buried in compact sediments such as
sand. A boomer or sparker should be the energy transmitting
source. The signals
from these sources
induce deeper pene-
tration. Lower fre-
quencies are useful
for obtaining better
penetration
in
the
sediments
of
sub-
bottom
formations
and those buried in
unconsolidated
sedi-
ments, but the prob-
lem is that the fea-
tures
are
recorded
only when the instru-
ment passes directly
over the object.