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Among these, the Shakti Peethas at Kamkhya, Gaya and Ujjain are regarded as most sacred as they symbolize three most important aspects of mother Goddess viz. When observed carefully one can see that they lie in a perfect straight line from Kamakhya to Ujjain via Gaya symbolizing that every creation in this universe will annihilate one day without fail. The temple is located in Trimkomali, or Trincomalee on the eastern coast of Sri Lanka. The place Trinconmalee means a triangular shaped hill Tri- cona- malee or malai. The temple is well connected by roads. There is also a Kali temple which people visit enroute to Shankari Devi temple. This Shloka enumerates the list of places of Devi temples which are considered to be part of the 18 Devi Peethas. But almost nobody in Sri Lanka knew of any famous Devi Temple in the country.

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Click here to download a PDF version of this webpage Summary The widely accepted mantle plume model e. Geological and geophysical data from the Deccan provide no support for the plume model and arguably undermine it altogether Sheth, a ,b. The interplay of several intersecting continental rift zones in India is apparently responsible for the roughly circular outcrop of the Deccan. Published Ar-Ar age data for the Lakshadweep-Chagos Ridge basalts have been seriously questioned Baksi, , , and geochemical data suggest that they likely represent post-shield volcanism Sheth et al.

I relate CFB volcanism to continental rifting, which often but not always evolves into full-fledged sea-floor spreading Sheth, a , a. Non-plume, plate tectonic models are capable of explaining the Deccan in all its greatness. The 1, m-thick exposed section through the Deccan basalt pile at Mahabaleshwar, Sahyadri Western Ghats region. Photo by Hetu Sheth. These papers are in unanimous agreement on two issues: Nevertheless, the following observations and deductions suggest that the plume model is not valid for the Deccan Sheth, a , b , a.

Map showing the approximate boundaries of the Precambrian cratons making up the Indian shield e. Inset shows the breakup of the Seychelles microcontinent, situated along the northern tip of the Mascarene Plateau black , from India, soon after the Deccan flood basalt episode after Norton and Sclater, ; Mahoney, Prominent structural-tectonic features of southern Asia and the Indian Ocean basin based on Mahoney et al. Abbreviations for localities are:

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Agriculture is one of the most important sectors in Telangana. Crops like cotton, mango and tobacco are locally grown in the state. With a focus on information technology and biotechnology, Telangana is one of the top IT exporting states of India. With the presence of the coal reserves in Singaerni Collieries, Telangana is also considered a mineral-rich state.

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History[ edit ] Along with much of present-day coastal Andhra Pradesh, Bhimavaram was controlled by the Chola dynasty. Under Kulothunga Chola I , Bhimavaram was ruled by his sons who served as viceroys. Stone inscriptions have been found in the town dating from his reign c. According to a legend, in around — AD, an Eastern Chalukya king named Chalukya Bheema built a Siva temple and laid the foundation to this town.

Demographics[ edit ] As of [update] census of India , the town had a population of , The total population constitutes 70, males and 72, females—a sex ratio of females per males.

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Paleontological studies of sediments adjacent to the basalt at depth in Krishna-Godavari Basin, e. However, plateau ages as precise as A petrogenetic link between these basalts and the Deccan Trap basalts the remains of which lie over km from the nearest exposure of Rajahmundry Trap has been suggested but has yet to be substantiated. These new data clearly place the eruption of the Rajahmundry Traps temporally close to the K-T boundary, coincident with late stage Deccan volcanism and within ca.

Paleomagnetic studies of Vandamme and Courtillot revealed a reverse to normal magnetization polarity sequence within the Rajahmundry Traps, supporting a temporal connection with waning of Deccan Trap volcanism, consistent with our results. This now unequivocal temporal connection between the Rajahmundry Traps and Deccan Traps may suggest a much larger area of melt generation beneath the Indian sub continent than previously estimated, or may be the result of extensive overland flow distances e.

The latter possibility would require significant paleovalleys to be maintained even after serving as conduits for, and presumably being filled by several individual flows, evidence of which is lacking. Recent reconstructions modeling the evolution of the Krishna-Godavari Basin and catchments clearly show that then, as now, this basin drains much of the Indian Peninsula, including the main Deccan Traps at their time of eruption Halkett, et al.

Overland flow of Deccan Trap volcanism thus remains a plausible origin for the Rajahmundry Traps.

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Recent rock quarries in Rajahmundry Trap lavas of basaltic composition have exposed fresh surfaces available for sampling displaying clear stratigraphic relationships within the typical basalt—sediment—basalt stratigraphy. These data indicate a lengthy hiatus between volcanism and subsequent deposition of Eocene sandstones, which locally overly the Rajahmundry sequences. These age data also place the eruption of the Rajahmundry Traps coincident with late-stage Deccan Trap volcanism.

This synchronicity is consistent with new geochemical data and published paleomagnetic evidence. Do you want to read the rest of this article? We emphasize that any starting condition could be used for inverse modeling and that inclusion of moderate topographic relief would be unlikely to dramatically alter our principal conclusions. A combination of stratigraphic relationships, incision patterns, and the great distances over which Paleocene lavas flowed, imply that eastward-directed drainage patterns were established by this time [Cox, ; Knight et al.

Deep incision of the Eastern Ghats region by eastward-flowing rivers provides corroborative evidence that these drainage patterns are probably antecedent and have therefore been relatively stable over a long period [Widdowson and Cox, ; Gunnell and Harbor, ].

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