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<title>Geography</title>
<link href="http://dr.lib.sjp.ac.lk/handle/123456789/21" rel="alternate"/>
<subtitle/>
<id>http://dr.lib.sjp.ac.lk/handle/123456789/21</id>
<updated>2026-04-23T10:25:00Z</updated>
<dc:date>2026-04-23T10:25:00Z</dc:date>
<entry>
<title>INSELBERGS IN VIJAYAN COMPLEX OF SRI LANKA</title>
<link href="http://dr.lib.sjp.ac.lk/handle/123456789/12926" rel="alternate"/>
<author>
<name>Katupotha, K.N.J.</name>
</author>
<author>
<name>Karunarathne, S.</name>
</author>
<author>
<name>Adikaram, M.</name>
</author>
<id>http://dr.lib.sjp.ac.lk/handle/123456789/12926</id>
<updated>2024-03-14T06:33:56Z</updated>
<published>2024-01-01T00:00:00Z</published>
<summary type="text">INSELBERGS IN VIJAYAN COMPLEX OF SRI LANKA
Katupotha, K.N.J.; Karunarathne, S.; Adikaram, M.
</summary>
<dc:date>2024-01-01T00:00:00Z</dc:date>
</entry>
<entry>
<title>හෙලොසීන අවධිය හා ශ්‍රී ලංකාවේ මුහුදු මට්ටමේ ඇති වු වෙනස්කම්</title>
<link href="http://dr.lib.sjp.ac.lk/handle/123456789/12925" rel="alternate"/>
<author>
<name>කටුපොත, ජි.</name>
</author>
<id>http://dr.lib.sjp.ac.lk/handle/123456789/12925</id>
<updated>2024-03-14T06:11:36Z</updated>
<published>2020-01-01T00:00:00Z</published>
<summary type="text">හෙලොසීන අවධිය හා ශ්‍රී ලංකාවේ මුහුදු මට්ටමේ ඇති වු වෙනස්කම්
කටුපොත, ජි.
</summary>
<dc:date>2020-01-01T00:00:00Z</dc:date>
</entry>
<entry>
<title>Fossil Diatom Assemblages and Pyrite Formation of the Post Glacial Stage and the Holocene Epoch in Fujii Area, Okayama Plain, Japan</title>
<link href="http://dr.lib.sjp.ac.lk/handle/123456789/12924" rel="alternate"/>
<author>
<name>Prasadika, H.K.A.E.</name>
</author>
<author>
<name>Katupotha, K.N.J.</name>
</author>
<author>
<name>Gamage, S.G.</name>
</author>
<id>http://dr.lib.sjp.ac.lk/handle/123456789/12924</id>
<updated>2024-03-14T04:59:56Z</updated>
<published>2023-01-01T00:00:00Z</published>
<summary type="text">Fossil Diatom Assemblages and Pyrite Formation of the Post Glacial Stage and the Holocene Epoch in Fujii Area, Okayama Plain, Japan
Prasadika, H.K.A.E.; Katupotha, K.N.J.; Gamage, S.G.
</summary>
<dc:date>2023-01-01T00:00:00Z</dc:date>
</entry>
<entry>
<title>Configuration of the Indian Ocean and location of Sri Lanka</title>
<link href="http://dr.lib.sjp.ac.lk/handle/123456789/12923" rel="alternate"/>
<author>
<name>Katupotha, J.</name>
</author>
<id>http://dr.lib.sjp.ac.lk/handle/123456789/12923</id>
<updated>2024-03-14T04:47:21Z</updated>
<published>2020-01-01T00:00:00Z</published>
<summary type="text">Configuration of the Indian Ocean and location of Sri Lanka
Katupotha, J.
The Indian Ocean is bounded by Iran, Pakistan, India, and Bangladesh to the north; the Malay&#13;
Peninsula, the Sunda Islands of Indonesia, and Australia to the east; Antarctica to the south; and Africa&#13;
and the Arabian Peninsula to the west. Island nations are located in the Indian Ocean, such as Comoros,&#13;
Madagascar, Maldives, Mauritius, Seychelles, and Sri Lanka. Likewise, it is home to hundreds of&#13;
islands. It has an area of about 73,440,000 square km. The Indian Ocean’s average depth is 3,960&#13;
metres, and its deepest point, in the Sunda Deep of the Java Trench off the southern coast of the island&#13;
of Java (Indonesia), is 7,450 metres. During the long span of time, since the Late Jurassic period&#13;
(152myr) to present., the formation, evolution and present configuration of the Indian ocean obtained its&#13;
inheritable characteristics, such as oceanic ridges and fracture zones, seamounts, ocean basins, trenches&#13;
and continental rise, slope, and shelf. Besides, several well-defined coastal morphological features are&#13;
found in the Indian Ocean: estuaries, deltas, salt marshes, mangrove swamps, cliffs, coral reefs, and&#13;
complexes of barrier islands, lagoons, beaches, and coastal dunes which are highly significance for ecoand geo-tourism. With the development and evolution of these phenomena in the Indian Ocean, the&#13;
island of Sri Lanka moves from Late Jurassic period to its present position. During the Upper Jurassic&#13;
Period Sri Lanka was positioned within 65o&#13;
S-67o&#13;
S and 32oE-36oE in the Indian Ocean, and with the Sri&#13;
Lanka detached from the southern supercontinent Gondwanaland, the Indian Ocean began to open up.
</summary>
<dc:date>2020-01-01T00:00:00Z</dc:date>
</entry>
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