Deep Water Tsunami Wave Monitoring System Presentation slide image

Deep Water Tsunami Wave Monitoring System Presentation

16 Q INDIA Colombo Northeast Indian Ocean Region Seismicity 1900 - 2004, M≥6 BAN H 106 CAINA. Kolkata (Calcutta) Dhaka MYANMAR 6B4RMA) Viangchan Vientiane) BAY OF BENCAL Yangon (Rangoon) THAILAND Krung Thep. Chennai (Madras) Andaman Is ✓ SRI LANKA Hanoi VIET Bangkok) AMBODIANA Anom Penh INDIAN OCEAN MALAYSIA Kuala Lumpur NGAPORE Singapore ONESIA 700 LO O ME Mudo Ago SUNCA TRENCH 1200 Koma Jakarta Historic Seismicity Eastern Indian Ocean 1900 - 2004 ■ The Indian Plate moves northeasterly about 60 mm/yr relative to the Burma Plate, resulting in oblique convergence with the Sunda Trench ■ The last major earthquake in the Sunda Trench was in southeastern Sumatra in 1833. The tsunamis generated by that quake were directed southerly, towards Antarctica. EXPLANATION Main Shock 26 December 2004 O Atershocks M 26 Earthquakes M≥6 0-69 km O 70 - 299 O 300-699 ▲ Volcanoes
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