The 2007 Solomon Islands earthquake took place on 2 April 2007, near the provincial capital of Gizo on Ghizo Island, in Solomon Islands. Sumatra was taken off tsunami alert after two hours. As high-magnitude ocean waves propagate at high speeds close to 25 meters per second, they traversed the 55-kilometer distance from the epicenter to Gavo in less than 20 minutes. There were numerou…
A tsunami approximately 1 metre high was reported at Padang, Indonesia. The tsunami that followed the earthquake killed 52 people. Our multimedia service, through this new integrated single platform, updates throughout the day, in text, audio and video – also making use of quality images and other media from across the UN system. The From Honiara, one of the first warnings came from the At least fifty-two people were reported to have been killed and sixty reported missing when a Australia committed to contribute an initial 3 million AUD in emergency aid, later increased to 5.7 million as of June 2007.Francis Billy Hilly, the MP for Simbo Island where 10 people died, said on 8 April that those who had previously resisted resettlement away from the island's active volcano were reconsidering their options. The The magnitude 7.9 earthquake was also a result of thrust faulting on the same plate boundary.
It occurred about 225 km northwest of the magnitude 8.4 earthquake, at the northern end of the aftershock zone.The magnitude 8.4 earthquake was the most powerful earthquake of 2007 to date, more powerful than the two The tsunami that was triggered by a magnitude 8.1 earthquake on April 1, 2007, in the Solomon Islands caused significant damage and loss of life. UN News produces daily news content in Arabic, Chinese, English, French, Kiswahili, Portuguese, Russian and Spanish, and weekly programmes in Hindi, Urdu and Bangla.
A total of 4 tsunami alerts were issued in 24 hours. The focus was 10 km (6 mi) deep and 40 km (25 mi) South South-East of Gizo township on New Georgia Islands in Western Province. The information presented here is focused on geologic aspects of the disaster. A small tsunami, some 15 cm high, was reported at the Cocos Islands. The shorter rupture (estimated roughly at about 200 km) and the smaller magnitude were the probable reasons for the smaller 2007 tsunami. After further aftershocks above magnitude 5, a third large earthquake, 7.0 Aftershocks continued into 13 September and 14 September, with more earthquakes ranging up to magnitude 6.4.Tremors were felt in neighbouring countries as far away as Tsunami warnings were also issued in India and other countries around the Indian Ocean soon after the earthquake. Its magnitude was estimated at 8.1 on the Mw scale, and 7.8 on the Ms scale. Sea level readings indicated that a tsunami was generated. In the hopes that disasters such as this can be avoided in the future, we attempt to understand the mechanism and impact of this tsunami. After the first, and largest, earthquake, the Pacific Tsunami Warning Centre issued a tsunami alert for much of the Indian Ocean basin. According to the USGS, the earthquake was recorded around 7:39:56 a.m. local time (UTC+11). Apparently, the September 12, 2007 earthquake had a smaller magnitude and length of rupture than the 1833 event which generated a much greater tsunami.
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