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Socio-cultural Processes and Livelihood Patterns at Tirurangadi - CDS

Socio-cultural Processes and Livelihood Patterns at Tirurangadi - CDS

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more detailed archeological <strong>and</strong> geological investig<strong>at</strong>ion into the area, which appears to<br />

have had commercial significance.<br />

Apart from the mainl<strong>and</strong> Kadalundi there are a number of thiruttis in the azhimukham,<br />

<strong>and</strong> the river takes several twists <strong>and</strong> turns around several l<strong>and</strong> form<strong>at</strong>ions before it<br />

finally joins the sea. One of these form<strong>at</strong>ions might have become the earlier habit<strong>at</strong>. And<br />

l<strong>at</strong>er the entire area came to be called Kadalundi. The tradition among the local people<br />

th<strong>at</strong> the original Kadalundi was the nagaram to the south of the river, <strong>and</strong> the central area<br />

shifted to the north of the river only recently, after the coming railway st<strong>at</strong>ion <strong>and</strong> the<br />

bridge will have to be taken seriously. Unfortun<strong>at</strong>ely, unlike Musiri or Kodungallur<br />

which had a long historical <strong>and</strong> <strong>cultural</strong> tradition <strong>and</strong> hence has <strong>at</strong>tracted the <strong>at</strong>tention of<br />

archeologists <strong>and</strong> historians alike, Thondi has just remained a name found in the early<br />

Tamil songs <strong>and</strong> roman notices, which has since disappeared. The historian <strong>and</strong> the<br />

archeologist are yet to make a serious study of the region.<br />

A few geological fe<strong>at</strong>ures of the area seem to be significant in this context. Geologists<br />

have shown th<strong>at</strong> the coastal area <strong>and</strong> a part of the interior region mainly consist of<br />

riverside alluvial soil th<strong>at</strong> has been formed recently. (Resource based perspective plan for<br />

2020AD, Karalla L<strong>and</strong> Use Board, 1997). The sea appears to have advanced <strong>and</strong> receded<br />

several times, <strong>and</strong> the river has also changed its course. Discovery of river s<strong>and</strong> <strong>and</strong><br />

seashells <strong>and</strong> other objects while digging wells may signify the early layers left by such<br />

advance <strong>and</strong> withdrawal. Hence it is not impossible to visualize a coastal form<strong>at</strong>ion<br />

different from th<strong>at</strong> of today <strong>and</strong> the existence of a port th<strong>at</strong> was loc<strong>at</strong>ed <strong>at</strong> the confluence<br />

of the river <strong>and</strong> the sea, of which Kadalundi Nagaram is the area th<strong>at</strong> has remained today.<br />

Perhaps the thiruttis th<strong>at</strong> we see today were also part of the same form<strong>at</strong>ion.<br />

Another fe<strong>at</strong>ure also appears to be significant. Adjacent to Kadalundi <strong>and</strong> in between the<br />

rivers of Chaliyar <strong>and</strong> Kadalundi, there appears to be a number of places where early<br />

terus or market centers may be loc<strong>at</strong>ed. Thus we have Idimuzhiikkal, Pallikkal

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