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Location of Lake Toba shown in red on map. The Toba eruption (the Toba event) occurred at what is now Lake Toba about 73,700±300 years ago. [15] It was the last in a series of at least four caldera-forming eruptions at this location, with the earlier known caldera having formed around 1.2 million years ago. [16]
The Toba eruption (also called the Toba supereruption and the Youngest Toba eruption) was a supervolcanic eruption that occurred about 74,000 years ago, during the Late Pleistocene, [2] at the site of present-day Lake Toba, in Sumatra, Indonesia.
The volume of a lake is a difficult quantity to measure. [1] Generally, the volume must be inferred from bathymetric data by integration. Lake volumes can also change dramatically over time and during the year, especially for salt lakes in arid climates.
Google Earth is a web and computer program that renders a 3D representation of Earth based primarily on satellite imagery.The program maps the Earth by superimposing satellite images, aerial photography, and GIS data onto a 3D globe, allowing users to see cities and landscapes from various angles.
Lake Toba Caldera: Sunda Arc, Sumatra 2,800 - 5,300 [13] 74 Youngest Toba Tuff [b] 6 Barrier Volcano: Great Rift Valley, Kenya: 10 74 caldera formation 6 Kuttara Hokkaidō > 11 DRE 75 Kt-4 6 Phlegraean Fields Campanian volcanic arc 12.35 80 CA-1a Tephra 6 Bolshoy Semyachik: Kamchatka: 42 80 Bol'shoi Semiachik Caldera II 6 Hakone: Honshū: 10
Erath is located at (29.959939, -92.035220 According to the United States Census Bureau, the town has a total area of 1.5 square miles (3.9 km 2), all land.. Erath is located 20 miles (32 km) south of Lafayette, parish seat of Lafayette Parish via Louisiana Highway 339, 7 miles (11 km) east of Abbeville, parish seat of Vermilion Parish, and 15 miles (24 km) west of New Iberia, parish seat of ...
[5] [6] The most recent is Lake Taupō's Oruanui eruption, more than 27,000 years ago, which means that there have not been any Holocene eruptions with a VEI of 8. [5] There have been at least 10 eruptions of VEI-7 in the last 11,700 years. There are also 58 Plinian eruptions, and 13 caldera-forming eruptions, of large, but unknown magnitudes.
A recursive island or lake, also known as a nested island or lake, is an island or a lake that lies within a lake or an island. [1] For the purposes of defining recursion, small continental land masses such as Madagascar and New Zealand count as islands, while large continental land masses do not. Islands found within lakes in these countries ...