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Ancient ports of Gujarat
The map shows that the area
northwest of Ahmedabad is covered by palaeo-mudflats. Modhera is presently
situated on the bank of the river Pushpavati on the edge of a paleo-mudflat.
Hence it means that the town was situated near the seacoast and hence might have
been a port at some time in the past. At the Bhavnagar coast, one can easily
make out that earlier the coastline was more towards the west. The area to the
east of the old coastline has come up, or the sea has receded later on, as it
shows a broad saline band and all the rivers end on the strand line. Most of the
rivers show wider river mouths near the strand lines, Figure 1. The location of
Vallabhi town falls on this strand line on the bank of the present Ghelo River.
The seacoast was not far away from the town. There are villages named Juni
Rajsthali and Navi Rajsthali near Vallabhi that might be the places of the
King’s residence or palace during those days.
Varahi, Benap and Tharad
are located on the bank of a palaeo-channel that might have been a mighty river
(Saraswati?) as the width of the palaeo-channel is very large. Thus these ports
might have been riverine ports in those days. Some of the ports might have
closed out due to unfavourable conditions. Mavsari, Padan, Amarapur, Kodadha,
Zinzuwada and Guntaligadh located on the bank of the Great Rann or the Little
Rann of Kachchha, which were once a part of the sea, are examples of such ports.
Thus, remote sensing data shows that most of the places mentioned in literature
which are believed to be the ports were indeed ports in the past. Thus it is
possible to find out or confirm the location of old riverine ports or seaports
using satellite data.
Table - 1 Ancient Ports of
Gujarat
|
Port |
Location |
Taluka/District |
Remarks |
|
|
Lat |
Long |
|
|
| 1 |
Desalpur \ Guntali gadh |
23o27’N |
69o10’E |
Nakhatrana Kachchha |
Excavation |
| 2 |
Rayan Mandavi |
22o53’N |
69o21’E |
Mandavi, Kachchha |
|
| 3 |
Bhadreshwar |
22o55’N |
69o54’E |
Anjar, Kachchha |
|
| 4 |
Koteshwar |
23o41’N |
68o32’E |
-do- |
|
| 5 |
Jungi |
23o13’N |
70o34’E |
Bhachau, Kachchha |
|
| 6 |
Tuna |
22o59’N |
70o05’E |
Anjar, Kachchha |
|
| 7 |
Mavsari |
24o37’N |
71o22’E |
Vav, Banaskantha |
|
| 8 |
Benap |
24o09’N |
71o25’E |
Vav, Banaskantha |
|
| 9 |
Amarapur |
23o36’N |
71o27’E |
Santalpur, -do- |
|
| 10 |
Padan |
24o18’N |
71o19’E |
-do- |
|
| 11 |
Boru |
24o02’N |
71o20’E |
Vav,Banaskantha |
|
| 12 |
Kodadha |
23o33’N |
71o30’E |
Sami, Mehsana |
Anchors found |
| 13 |
Modhera |
23o35’N |
71o08’E |
Becharaji, Mehsana |
|
| 14 |
Kamboi |
23o41’N |
72o02’E |
Chanasma, -do- |
temple of Vahanvati Goddess |
| 15 |
Zinzuwada |
23o21’N |
71o39'E |
Dasada, Surendranagar |
Anchors |
| 16 |
Kuntasi |
22o54’N |
70o36’E |
Maliya, Rajkot excavation |
| 17 |
Hajnali |
22o52’N |
70o37’E |
-do- |
|
| 18 |
Dahisar |
22o57’N |
70o37’E |
-do- |
|
| 19 |
Khakharechi |
23o05’N |
70o55’E |
-do- |
|
| 20 |
Vavania |
23o00’N |
70o55’E |
-do- |
established 1763AD |
| 21 |
Pindara |
|
|
Jamnagar |
|
| 22 |
Vallabhi |
21o53’N |
71o53’E |
Bhavnagar |
|
| 23 |
Vartej |
21o44’N |
72o04’E |
-do- |
|
| 24 |
Lothal |
22o31’N |
72o15’E |
Ahmedabad excavation |
|
| 25 |
Dholera |
22o15’N |
72o11’E |
-do- |
|
| 26 |
Nagara |
22o22’N |
72o37’E |
Kheda |
5th BC Excavation |
| 27 |
Khambhat |
22o18’N |
72o37’E |
-do- |
|
| 28 |
Bharuch |
|
|
Bharuch |
500BC |
| 29 |
Rander |
21o13’N |
72o47’E |
Surat |
|
| 30 |
Bilimora |
20o47’N |
72o58’E |
Valsad |
Mediaval |
| 31 |
Varahi |
23o47’N |
71o27’E |
Santalpur, Banaskantha |
|
| 32 |
Mahuva |
21o05’N |
71o46’E |
|
|
| 33 |
Surat |
21o12’N |
72o50’E |
Surat |
|
| 34 |
Kanakpur (Katpur?) |
21o02’N |
71o48’E |
|
|
| 35 |
Navsari |
20o57’N |
72o55’E |
Valsad |
841 AD |
| 36 |
Tharad |
24o24’N |
71o38’E |
Banaskantha |
|
| 37 |
Gandhar |
21o53’N |
72o39’E |
Bharuch |
| An Attempt to Locate
New SitesNew sites of archaeological interest can be located using soil
marks, vegetation marks and anomalous landforms from the satellite data. New
sites can be found out on the old seacoast, palaeo mudflats or present coast or
in the old seabeds. An attempt has been made to find out whether any such sign
is there in the Rann of Kachchha or not. It is reported that the river Saraswati
was flowing along the bank of the Little Rann of Kachchha and pouring its water
in the Gulf of Khambhat. It is also reported that the river Saraswati was
flowing in Kachchha up to 325 BC. The flow of the river Saraswati has been shown
in Gujarat through the Rann of Kachchha up to Saurashtra from north Gujarat.
Kota Venkatachelam has also shown the river Saraswati pouring water in the Rann.
Figure 6 shows the map from ‘Ancient Bharat Varsha’ showing the flow of river
Saraswati up to the Great Rann of Kachchha. In view of this and the recent
findings at Dholavira, an attempt has been made to locate the possible sites of
ancient ports. The Great Rann of Kachchha which is dry Rann having
encrusted salt in the dry season was examined in the satellite imagery. During
monsoon the same area is covered with water. The area was part of the sea for
more than 1000 years. IRS Geo-coded data of this area representing the Survey of
India Toposheet no. 40L\8 was selected for site location. The image shows signs
of a mighty river (Saraswati?) flowing in this area. River flow is between
70o 15' - 70o 30' E, the flow is north to south in direction and shows a
bifurcation. The other signs show that there might be probable sites of towns or
villages, at about 24o 09' N and 70o 28' E, 24o 13' N and 70o 16' E, 24o 02' N
and 70o 29' E. A water body at 24o 09' N and 70o 17' E could be a village tank.
Agricultural areas can be seen between 24o 11' - 24o 15' N and
70o 20' - 70o 30' E. SOI Toposheet shows only dry Rann having only one island,
Maruda Takkar, having 23m height. The other information given is salt waste and
the area remains usually flooded during July to December. Such signs can
also be seen in the south of Jakhel village, in between Jakhel and Chadiyana of
Sami taluka. Some anomalous structures can also be seen in the north west of
Subapura village of Sami taluka Mehsana district. (SOI toposheet no.41 M/10.) A
more detailed survey is required for further confirmatory information. It would
be useful if some of these sites could be investigated further to verify the
indications seen in the satellite data. ConclusionThus remote
sensing technology can play an important role in understanding the past in the
context of available historical and ancient literature. Remote sensing data can
successfully be used for building up historical records and changes that might
have taken place on the surface of the earth in the past. The data may also be
used for upgrading historical atlases, which might have been prepared using only
limited knowledge, and as per the imagination of certain scholars. The
proper planning, use and application of remote sensing techniques in archaeology
will result in economic benefits through reduction of costs of survey. Remote
sensing technique can increase efficiency, speed and data extraction at all
stages of archaeological research. Aided by the broad, interdisciplinary scope
injected by remote sensing data, archaeology may, in the near future, transcend
its traditional narrow focus. This may, in fact, be one of the best
justifications for a public, and publicly funded, remote sensing based
archaeology programme.
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