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Dating cest toc

dating cest toc-41

The goal of this movement was to establish an Islamic nation in Indonesia. More spectacularly, there was 10 m (33 ft) movement laterally and 4–5 m (13–16 ft) vertically along the fault line.

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For Indonesian A1 Grand Prix on November 2008, the government have been developing Lippo Karawaci circuit. The shock waves of the earthquake were felt across the planet; as far away as the U. state of Oklahoma, where vertical movements of 3 mm (0.12 in) were recorded. One can find any food and all things Chinese there. Other aftershocks of up to magnitude 6.6 continued to shake the region daily for up to three or four months.[18][19] As well as continuing aftershocks, the energy released by the original earthquake continued to make its presence felt well after the event. Lippo Karawaci, Bintaro Jaya, Bumi Serpong Damai and Alam Sutra are new locations of residential places (New Towns). A week after the earthquake, its reverberations could still be measured, providing valuable scientific data about the Earth’s interior. * “Italy History – Italian History Index” (in Italian, English). A vast majority of the residents are newcomers, not genuine Benteng Chinese. The 2004 Indian Ocean earthquake came just three days after a magnitude 8.1 earthquake in an uninhabited region west of New Zealand’s sub-Antarctic Auckland Islands, and north of Australia’s Macquarie Island. Geological Survey sees no evidence of a causal relationship in this incident. European University Institute, The World Wide Web Virtual Library. [edit] Infrastructure and Facility Metropolis, one of the modern city which is being developed by the government of Tangerang There are two highway connections from Jakarta. This is unusual, since earthquakes of magnitude 8 or more occur only about once per year on average.[20] Some seismologists have speculated about a connection between these two earthquakes, saying that the former one might have been a catalyst to the Indian Ocean earthquake, as the two earthquakes happened on opposite sides of the Indo-Australian Plate. Coincidentally, the earthquake struck almost exactly one year (to the hour) after a 6.6 magnitude earthquake killed an estimated 30,000 people in the city of Bam in Iran on December 26, 2003.[21] Some scientists confirm that the December earthquake had activated Leuser Mountain, a volcano in Aceh province along the same range of peaks as Mount Talang, while the 2005 Sumatran earthquake had sparked activity in Lake Toba, an ancient crater in Sumatra.[22] Geologists say that the eruption of Mount Talang in April 2005 is connected to the December earthquake.[23] Energy released The energy released on the Earth’s surface only (ME, which is the seismic potential for damage) by the 2004 Indian Ocean earthquake and tsunami was estimated at 1.1×1017 joules,[24] or 26.3 megatons of TNT. * “Fasti Online: A database of archaeological excavations since the year 2000”. In an effort to increase regional economic growth necessary first known or potential resources of a region can be expected to develop optimally. The seismograms are arranged vertically by distance from the epicenter in degrees.

This study is an effort to identify potential areas that have a big impact on economic growth in the area of the city Tangerang during the year 2001 until the year 2004, and how much contribution of these potential sectors to local economic growth. The earliest, lower amplitude, signal is that of the compressional (P) wave, which takes about 22 minutes to reach the other side of the planet (the antipode; in this case near Ecuador).

Certain areas consist of swamps, including the areas near the Soekarno-Hatta International Airport. The volcanic activity that results as the Indo-Australian Plate subducts the Eurasian Plate has created the Sunda Arc.

In recent years the urban expansion of Jakarta has covered Tangerang, and as a result many of its residents commute to Jakarta for work, or vice-versa. ^ “Transportation Issues and Future Condition in Tokyo, Jakarta, Manila and Hiroshima” (PDF). As well as the sideways movement between the plates, the sea floor is estimated to have risen by several metres, displacing an estimated 30 km3 (7 cu mi) of water and triggering devastating tsunami waves.

Many high-class and middle-class satellite cities have been developed in Tangerang, complete with their own shopping malls, private schools and convenience centers. The waves did not originate from a point source, as was inaccurately depicted in some illustrations of their paths of travel, but rather radiated outwards along the entire 1,600 km (994 mi) length of the rupture (acting as a line source).

The government is working on expanding the highway system to accommodate more traffic flow to and from the area.[citation needed] [edit] Demographics Tangerang also has a significant community of Chinese Indonesians, many of whom are of Cina Benteng extraction. They were descended from laborers who were brought there by the Dutch colonials in the 18th and 19th centuries, and most of them are still laborers and farmers. This greatly increased the geographical area over which the waves were observed, reaching as far as Mexico, Chile, and the Arctic.

On October 31, 1945, Laskar Hitam kidnapped Otto Iskandardinata, Republic of Indonesia’s Minister of State. ^ “Condemned Communities: Forced Evictions in Jakarta” Human Rights Watch Sep 2006. The Andaman and Nicobar Islands appear to have shifted south-west by around 1.25 m (4.1 ft) and to have sunk by 1 m (3.28 ft).[32] In February 2005, the Royal Navy vessel HMS Scott surveyed the seabed around the earthquake zone, which varies in depth between 1,000 m and 5,000 m (3,300 ft and 16,500 ft).