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The 2024 Kuala Lumpur sinkhole, also known as the Jalan Masjid India sinkhole, is a 8-metre (26 ft) deep sinkhole which formed in Jalan Masjid India in Kuala Lumpur on the 23rd of August 2024, possibly caused by sewage pipe ruptures and other geographical faults. [3][4] Its collapse has caused one victim to disappear for more than a week. [5][6 ...
August 31, 2024 at 7:48 PM. Malaysian authorities have stopped a nine-day effort to find and rescue a woman who fell into a sinkhole in Kuala Lumpur, officials said Saturday. The operation will ...
August 29, 2024 at 10:56 AM. KUALA LUMPUR, Malaysia (AP) — The search for an Indian tourist who was swallowed by a sinkhole in Malaysia's capital entered a seventh day Thursday, with the ...
August 23, 2024 at 7:42 AM. An Indian woman fell into an 8m-deep sinkhole in Kuala Lumpur after a pavement caved in, Malaysian authorities said. The incident happened in the Dang Wangi area of the ...
Talk:2024 Kuala Lumpur sinkhole is part of WikiProject Geology, an attempt at creating a standardized, informative, comprehensive and easy-to-use geology resource. If you would like to participate, you can choose to edit this article, or visit the project page for more information.
The Fire and Rescue Department of Malaysia (Malay: Jabatan Bomba dan Penyelamat Malaysia (JBPM), Jawi: جابتن بومبا دان ڤڽلامت مليسيا ), commonly known as Bomba, is a federal agency of Malaysia responsible for firefighting and technical rescue. Bomba is a Malay word derived from the Portuguese bombeiros which means ...
60 km/h. The Stormwater Management And Road Tunnel (SMART Tunnel), E38, is a storm drainage and road structure in Kuala Lumpur, Malaysia, and a major national project in the country. The 9.7 km (6.0 mi) tunnel is the longest stormwater drainage tunnel in Southeast Asia and second longest in Asia. The main objective of this tunnel is to solve ...
The following is a list of sinkholes, blue holes, dolines, crown holes, cenotes, and pit caves. A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. Some are caused by karst processes—for example, the chemical dissolution of carbonate rocks [1] or suffosion processes. [2]