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Liyue represents the China-inspired region in Genshin Impact. The Geo-elemental nation is located in the eastern part of Teyvat and is the oldest established nation on the continent. [1] According to the lore, about 3,700 years ago, Rex Lapis founded Liyue. [2] The goddess Guizhong guarded Mt. Tianheng and built the Guizhong Ballista. [3]
The player may freely explore an open-world map. Here Aether, the male Traveler, is seen gliding, but the player can switch to other party members. Genshin Impact is an open-world, action role-playing game that allows the player to control one of four interchangeable characters in a party. [4]
The characters of Genshin Impact have enjoyed positive reception, especially in terms of revenue: as Genshin Impact is a gacha game, much of its revenue comes from sales of in-game currency players use to obtain characters. Most revenue comes from limited character banners.
MiHoYo Co., Ltd. [note 1] is a Chinese video game development and publishing company founded in 2012 and headquartered in Shanghai.The company is best known for developing the Honkai series, Tears of Themis, and Genshin Impact.
Paimon (Chinese: 派蒙; pinyin: Pàiméng) is a character from Genshin Impact, a 2020 action role-playing gacha game developed by miHoYo.She serves as the game's mascot, the player's guide, and icon for the game and official website.
Baltis Vallis / ˈ b ɔː l t ɪ s ˈ v æ l ɪ s / is a sinuous channel on Venus ranging from 1–3 km (0.62–1.86 mi) wide and ~6,800 km (4,200 mi) long, slightly longer than the Nile and the longest known channel of any kind in the Solar System. It is thought the channel once held a river of lava.
Uzboi Vallis is believed to have been formed by running water. It is believed that layers were formed on the floor of Uzboi Vallis (as shown in the HiRISE image below) when drainage was blocked by the impact that formed Holden Crater to the north. Eventually the lake in the area of Uzboi Vallis went high enough to overtop the rim of Holden. [2]
Impact craters generally have a rim with ejecta around them, in contrast volcanic craters usually do not have a rim or ejecta deposits. As craters get larger (greater than 10 km in diameter) they usually have a central peak. [27] The peak is caused by a rebound of the crater floor following the impact. [18] Sometimes craters will display layers.
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