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Two new playable races were added to World of Warcraft in The Burning Crusade: the Draenei of the Alliance and the Blood Elves of the Horde.Previously, the shaman class was exclusive to the Horde faction (available to the orc, troll and tauren races), and the paladin class was exclusive to the Alliance faction (available to the human and dwarf races); with the new races, the expansion allowed ...
World of Warcraft Classic is a 2019 massively multiplayer online role-playing game developed and published by Blizzard Entertainment. Running alongside the main version of the game , Classic recreates World of Warcraft in the vanilla state it was in before the release of its first expansion , The Burning Crusade .
Warcraft III: The Frozen Throne is the expansion pack for Warcraft III: Reign of Chaos, a real-time strategy video game by Blizzard Entertainment. It was released worldwide on July 1, 2003, for Microsoft Windows and Mac OS X. The Frozen Throne builds upon the story of Reign of Chaos and depicts the events after the main game's conclusion.
Warcraft III: Reforged is a remastered edition of the 2002 real-time strategy video game Warcraft III: Reign of Chaos and its expansion The Frozen Throne.Released on January 28, 2020, it adds revamped graphics, new campaign gameplay settings as well as modern online Battle.net features.
Two supporting tie-in novellas were published by Blizzard, both in hardcover and on the World of Warcraft website: [15] Elegy, by Christie Golden, tells the story from the Alliance perspective; and A Good War, by Robert Brooks, tells the story from the Horde perspective.
Frost weathering is a collective term for several mechanical weathering processes induced by stresses created by the freezing of water into ice. The term serves as an ...
A Viking ring fortress, Trelleborg-type fortress, or trelleborg (pl. trelleborgs), is a type of circular fort of a special design, built in Scandinavia during the Viking Age. These fortresses have a strictly circular shape, with roads and gates pointing in the four cardinal directions.
The frost line—also known as frost depth or freezing depth—is most commonly the depth to which the groundwater in soil is expected to freeze. The frost depth depends on the climatic conditions of an area, the heat transfer properties of the soil and adjacent materials, and on nearby heat sources.