More Knowlage About Indonesia

The important Indonesian islands are described by thoroughly wooded volcanic mountains inside that inclination that descends to the beach front fields covered by thick alluvial swamps that, therefore, are broken into shallow oceans and coral reefs. Under this surface, the interesting and complex real construction of Indonesia includes the intersection of three significant segments of the outer layer of the earth and includes a confusing series of racks, volcanic mountain chains and remote oceanic channels. The island of Borneo and the circular segment of the island that incorporates Sumatra, Java, Bali and the Sounda Minor chain sit on the Sunday platform, a southern expansion of the continental mass of Asia.

The shelf is limited in the south and west by remote oceanic channels, for example, the Java trench (around 24,440 feet [7,450 meters] deep in its absolute background), which structure the continental genuine limit. New Guinea and its neighboring islands, which possibly includes the island of Halmahera, sit on the Sahul shelf, which is an expansion of the northwest of the Australian continental mass; The shelf is limited to the upper part of the East by a progression of the maritime box and to the northwest by box, a chain of coral reef and a progression of submarine edges. The third important unit of the outer layer of the earth in Indonesia is an expansion of the mountain belt that structures Japan and the Philippines; The mountains run south between Borneo and New Guinea and incorporate a progression of volcanoes and remote oceanic channels near Celebes and Las Molucas.

The connection between these three extensions of land is not obviously perceived. The current developments of the Earth’s Ocean are quite misleading in the light of the fact that the oceans found in the Sunda and Sahul racks are shallow and geographically late onset; They lie in the continental dough instead of a genuine depth of the sea. The Sunday shelf near the Java Sea has moderately low relief, contains some coral reefs and is not volcanic. The framework of the mountain that extends along the oceans of southern China and celebrities of this shelf and denotes the outer edge of the continental mass of Asia, however, it is a solid relief area and is one of the More dynamic volcanic areas on the planet.

The outer side (south) of the island chain from Sumatra through Java and the lower structures the main edge of the land extension of Southeast Asia. It is described by dynamic volcanoes, limited to the south and west by a progression of remote oceanic channels. On the inner side (north) of the islands, the volcanic mountains are described in swamps, swamps and the Shash Java Sea. This protected ocean was molded at the end of the Pleistocene era (a long time ago), and there are tests of previous land sections, which worked with the relocation of plants and creatures of the Asian continent.

SUNDA shelf islands
Borneo is the third largest island on the planet and the primary island on the Sunday shelf. Mount Kinabalu, the highest top of the Southeast Asian archipelago, is not in Indonesia. It amounts to 13,455 feet (4,101 meters) in the northeast corner of the island, in the territory of Sabah. In any case, the relief of the island only occasionally exceeds 5,600 feet (1,700 meters), and most of the island falls by less than 1,000 feet (300 meters). Primary patterns are not characterized too much as in the nearby islands, although a wide mountain frame (which incorporates Mount Kinabalu) usually from the east superior to the southwest. Kalimantan, which includes around three quarters of the island, generally includes undulating swamps, with alluvial swamps near the coast and the mountains wrapped in the deep interior.

Riau Islands deceived East Sumatra, close to the southern outlet of the Malacca Strait. These islands have a stone center and can be seen as an expansion of the actual Malay Peninsula. Except for certain high countries in the western and southern regions, Riau Bunch islands generally consist of lowland landscapes. Sumatra across the equator, extending from northwest to southeast with more than 1,000 miles (1,600 km), with the most extreme width (calculating sea island) exactly 325 miles (525 km). It was flanked at the external edge (western) by non -volcanic island lines, including Simeulue, Nias, and Bunch Mentawai, there was no thick population.

The central area of ​​Sumatra is separate into four fundamental actual districts: a tight coast front plain throughout the western; The mountains of ranks, which expand the length of the island near the western edge and combine various dynamic volcanoes; The nonvolcanic zone into the low slopes that review down to the steady foundation of the Asian Central Region; And a large alluvial swamp, lying like 100 feet (30 meters) above sea level, it is the eastern part of the island. Most of the East Swamp is a humid hamlet that is difficult to enter.

Java exactly 660 miles (1,060 km) and has the largest width of around 125 miles (200 km). The actual division is not too wrong like the Sumatran, on the grounds that the mainland rack dropped sharply to the Indian Ocean in the southern part of the island. Java can be isolated into five Latitudinal physiographic districts. The main district, the development of the limestone stage, reaches along the southern coast; In certain areas, these stages arranged a local karst that is dissolved (eg., Separated by a sink mixed with an unexpected edge, unexpected rock, cave, and underground flow) that makes travel and residence a problem.

The mountain belt is right north, in the western fragment of the island, forming the next district; It is somewhat made from mud from dissolved volcanoes and combining various alluvial bowls that are developed strongly, especially around the urban community of Bandung and Garut. The volcanic belt that passes through the focal point of the island is the third district; It contains about 50 dynamic cones and nearly 20 volcanoes that have been emitted since the turn of the twenty hundred years. Northern alluvial belt, the fourth district, spread across the Sundanese rack towards the sea and stretched by the development of delta, especially during the volcanic movement. There is a deep inland expansion from this Alluvial district, which is in the slicer of focal Java to the southern coast. Finally, there is the second stage of the limestone stage along the North Madura bank (an island off the northeast coastline of Java) and a close segment from East Java.

The numerous islands of the minor Sundas to eastern Java are much more modest, less thick and less created than Java. The geography of Bali and Lombok is like that of eastern Java. The minor Sunday islands pass through Sumbawa and Flores, logically restricting until they appear in a guide like a spine of volcanic islands that surround the east towards the east towards the band islands. A similar volcanic framework returns in northern Celebes. Sumba and Timor structure an outer edge (south) of the non -volcanic islands that resembles the chain outside the western edge of the Sunday platform near Sumatra.

Sahul shelf islands
The Sahul shelf islands seem to have a physiographic structure like those of the Sunday shelf. They incorporate the Molucas del Norte and New Guinea. The Western New Guinea piece consists of the Indonesian territories of Papua and Western Papu of the nation. The two territories cover a distant place with a fabulous and deferred scene. The swamps of the mangroves seal a large part of the southern and western coast, while the Maoke mountains, including Jaya Peak, which at 16,024 feet (4,884 meters) is the most notable point in Indonesia, structures a characteristic impediment in the focal region . There is a plain front of Limitada beach in the north. A large part of the district is strong forest.

Tags: ,
Leave your comment
Comment
Name
Email