Thailand to scrap all emergency provisions as it seeks to boost a very fragile economic recovery
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16
Rescue Efforts Continue in Bangkok as Scanner Detects 70 Signs of Life
When you build a house of cards, any vibration will make it collapse. My comments - pasted from another thread. Bangkok sits on a different Geological setting than much of Thailand - it young soft sedimentary basin of softer rock... when a quake passes through the earths hard core, it is amplified in this basin setting - much like shaking a bowl of jelly, whereas the energy in other geological settings has been dissipated. Seismologists sometimes call this problem the "Mexico City Effect" and Bangkok is often used as another example in modern textbooks because the physics are almost the same . As a comparison this what the substrata of major Thai cities is made up of: Bangkok: Age of Sediment: Holocene (up to 10,000 years old) Characteristics: Soft clay, young alluvial deposits, thick layers (over 100 meters) Stability: Low (high seismic amplification) Pattaya: Age of Rocks: Mesozoic (65–250 million years old) Characteristics: Sandstone, siltstone, shale, crystalline basement rocks, igneous intrusions Stability: Moderate (more stable than Bangkok) Kanchanaburi: Age of Rocks: Paleozoic to Mesozoic (250–540 million years old) Characteristics: Limestone, sandstone, shale, igneous and metamorphic rocks Stability: High (geologically stable) Hua Hin: Age of Rocks: Paleozoic to Mesozoic (65–540 million years old) Characteristics: Sandstone, limestone, granite intrusions Stability: High (less risk of seismic amplification) Khon Kaen: Age of Rocks: Mesozoic (65–250 million years old) Characteristics: Sandstone, shale, siltstone (Khorat Plateau) Stability: Moderate (stable foundation compared to Bangkok) Chiang Mai: Age of Rocks: Paleozoic to Mesozoic (65–540 million years old) Characteristics: Igneous, metamorphic, and sedimentary rocks, including granite, schist, and limestone Stability: High (rugged, mountainous terrain with hard rock base) To avoid any comments that there is blame against Thailand that its capital was 'built' on a poor geological setting' consider ancient settlement theory, access to shipping, lowest bridging points etc... and the fact that at the time little was known of quakes or the area's geological setting. There are plenty of other major cities around the world are that at similar or greater 'amplification risk' from an earthquake due to their geological settings. Los Angeles, USA: Located on the Los Angeles Basin (soft alluvial sediments); ~50 km from the Pacific-North American Plate boundary (San Andreas Fault). Salt Lake City, USA: Situated on soft lake bed sediments from ancient Lake Bonneville; ~400 km from the Intermountain Seismic Belt (within the North American Plate). Seattle, USA: Built on the Seattle Basin (soft alluvial and sedimentary layers); ~100 km from the Juan de Fuca-North American Plate boundary (Cascadia Subduction Zone). Santiago, Chile: Located in the Santiago Basin (soft sedimentary deposits); ~100 km from the Nazca-South American Plate boundary. Quito, Ecuador: Built on soft volcanic ash deposits and sedimentary basins; ~200 km from the Nazca-South American Plate boundary. Athens, Greece: Built on soft alluvial deposits in some areas; ~100 km from the Hellenic Arc (African-Eurasian Plate) boundary. Istanbul, Turkey: Partly located on soft, young sediments near the Sea of Marmara; ~20 km from the North Anatolian Fault (Eurasian-Anatolian Plate boundary). Kathmandu, Nepal: Situated in the Kathmandu Valley (soft ancient lake sediments); ~50 km from the Indian-Eurasian Plate boundary (Himalayan Frontal Thrust). Tehran, Iran: Built on alluvial deposits and loose sediments from nearby mountains; ~100 km from the Arabian-Eurasian Plate boundary (Zagros Fold and Thrust Belt). Tokyo, Japan: Located in the Kanto Basin (soft sedimentary layers); ~100 km from the Pacific-Eurasian-Philippine Sea Plate junction. Taipei, Taiwan: Built on the Taipei Basin (thick sedimentary deposits); ~50 km from the Eurasian-Philippine Sea Plate boundary. Shanghai, China: Located on soft deltaic sediments from the Yangtze River; ~1,200 km from the Pacific-Eurasian Plate boundary (Japan Trench). Wellington, New Zealand: Built on soft alluvial sediments and reclaimed land; ~30 km from the Pacific-Australian Plate boundary (Wellington Fault). Cairo, Egypt: Partly built on Nile Delta sediments (soft, unconsolidated deposits); ~1,000 km from the African-Arabian Plate boundary (Red Sea Rift). -
11
Advice for married resident (ret visa) returning to Thailand on May 1st after 2 weeks away.
Obviously a very serious question Mr. Now it All. But thanks for the link. -
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Investors are stunned after the stock market closed its worst quarter in 3 years
Really. Why don't you debunk my points then in a logical fashion? I'm a trained economist btw so I'd say I'm not clueless. -
38
THAILAND LIVE Thailand Live Wednesday 2 April 2025
Phuket Prepares for Alcohol-Free Songkran Festivities on April 13 Photo courtesy of The Phuket News Phuket is set to host its annual alcohol-free Songkran festival next Sunday, April 13, offering a vibrant celebration of traditional activities, cultural performances, and live music in a family-friendly environment. This event not only commemorates Songkran's cultural heritage but also supports local tourism and businesses. Full Story: https://aseannow.com/topic/1356570-phuket-prepares-for-alcohol-free-songkran-festivities-on-april-13/ -
18
Dem-backed Susan Crawford wins Wisconsin Supreme Court seat, cementing liberal majority
Says the who trash talks fired government workers repeatedly. -
5
Transport Minister Orders Thorough Check of Thai-Chinese High-Speed Rail
Hope you got one for yourself too probly will become a collectors item must keep the box though.
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