1914 Whakaari-White Island | |
|---|---|
| Total costs | N/A |
| Deaths | 10 |
Whakaari / White Island ([faˈkaːɾi]), commonly known as White Island or Whakaari, is an active andesite stratovolcano situated 48 km (30 mi) from the east coast of the North Island of New Zealand, in the Bay of Plenty. The island covers an area of approximately 325 ha (800 acres), which is only the peak of a much larger submarine volcano. The island is New Zealand's most active cone volcano, and has been built up by continuous volcanic activity over the past 150,000 years. The nearest mainland towns are Whakatane and Tauranga. The island has been in a nearly continuous stage of releasing volcanic gas at least since it was sighted by James Cook in 1769. Whakaari erupted continually from December 1975 until September 2000, marking the world's longest historic eruption episode, according to GeoNet, and also in 2012, 2016, and 2019. Sulphur was mined on the island until the 1930s. Ten miners were killed in 1914 when part of the crater wall collapsed. The main activities on the island now include guided tours and scientific research. Access to the island is allowed only as a member of a tour run by a registered tour operator. A large eruption occurred at 14:11 on 9 December 2019, which resulted in 22 fatalities, including two people who were missing and ruled to be dead by a coroner. Twenty-five survivors were seriously injured, many critically and suffering severe burns. Three survivors suffered minor injuries. Forty-seven people were reportedly on the island when it erupted. A second eruption closely followed the first.
Source: Wikipedia 1864 Calcutta Cyclone | |
|---|---|
| Total costs | N/A |
| Deaths | 60000 |
On October 5, 1864, most of the areas of Calcutta (present-day Kolkata), India was inundated and destroyed by a tropical cyclone. Dubbed the 1864 Calcutta cyclone, the storm caused over 60,000 fatalities in its wake. The cyclone crossed the coast of West Bengal to the south of Hooghly River, one of the streams that are included in the Ganges River Delta. The majority of the deaths were from drowning and the others from sicknesses prevailing before the storm. The said river overflowed due to a storm surge and as the water rushed inland, everything in its course were washed away. The city, the other surrounding areas, and some harbors had to be rebuilt after the cyclone. There was also fundraising event established, but it failed. The total damages from the said storm were at Rs 99,200.
Source: WikipediaMount Sinabung (Indonesian: Gunung Sinabung, Karo: Deleng Sinabung) is a Pleistocene-to-Holocene...
The Persian plague epidemic of 1772–1773, also simply known as the Persian Plague, was a massive...
Taal Volcano (IPA: [taʔal]; Tagalog: Bulkang Taal) is a large caldera filled by Taal Lake in the...
The 1792 Unzen earthquake and tsunami resulted from the volcanic activities of Mount Unzen (in...
Welcome to 