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Old School RuneScape is a massively multiplayer online role-playing game (MMORPG), developed and published by Jagex.The game was released on 16 February 2013. When Old School RuneScape launched, it began as an August 2007 version of the game RuneScape, which was highly popular prior to the launch of RuneScape 3.
A volcanic fissure and lava channel with lava fountain Channel of lava erupted during a fissure eruption of Kīlauea volcano, Hawaii, 2007 Eruption fissure with spatter cones, Holuhraun, Iceland, 2014 Mauna Loa with different lava flows and fissure vent A volcanic fissure eruption on Fagradalsfjall, Iceland, 2021 Crater row of Laki Eldhraun, a lava field produced by the Laki craters Cinder ...
The game was released in March 2011. A port of the game, called Rift Mobile, was released for Android on January 25, 2012. Rift received generally positive reviews from game critics. In August 2011, Trion announced that 1 million users/players have played the game [1] and by January 2012 it had earned $100 million in total revenue. [2]
East Rift Zone on Kīlauea, Hawaiʻi. A rift zone is a feature of some volcanoes, especially shield volcanoes, in which a set of linear cracks (or rifts) develops in a volcanic edifice, typically forming into two or three well-defined regions along the flanks of the vent. [1]
Chimborazo has a circumference of 78 miles (126 km) and a diameter of 30 miles (48 km). Chimborazo's upper elevations are covered in glaciers that are decreasing in size due to climate change and falling ash from the nearby volcano, Tungurahua. In addition to the glaciers, the volcano is covered with craters.
The volcano erupted from 1983 to 2018 and is part of the Hawaiian–Emperor seamount chain. Mauna Loa is a large shield volcano. Its last eruption was in 2022 and it is part of the Hawaiian–Emperor seamount chain. Bowie Seamount is a dormant submarine volcano and part of the Kodiak-Bowie Seamount chain.
The central volcano has a rim that rises to about 2,000 m (6,600 ft) above sea level, [a] making it the second highest mountain in Iceland, being lower than Hvannadalshnjúkur. The caldera is about 65 km 2 (25 sq mi), [ 1 ] up to 10 km (6.2 mi) wide and about 700 m (2,300 ft) deep.
Teide's base is situated in Las Cañadas crater (the remains of an older, eroded, extinct volcano) at a height of around 2,190 m (7,190 ft) above sea level. Teide is an active volcano: its most recent eruption occurred in late 1909 from the El Chinyero vent on the northwestern Santiago rift. [11]