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Faerûn (/ f eɪ ˈ r uː n / fay-ROON) is a fictional continent and the primary setting of the Dungeons & Dragons world of Forgotten Realms.It is described in detail in several editions of the Forgotten Realms Campaign Setting (first published in 1987 by TSR, Inc.) with the most recent being the 5th edition from Wizards of the Coast, [1] [2] and various locales and aspects are described in ...
Abeir-Toril is the fictional planet that makes up the Forgotten Realms Dungeons & Dragons campaign setting, as well as the Al-Qadim and Maztica campaign settings, and the 1st edition version of the Oriental Adventures campaign setting.
Player's Guide to Faerûn is a collection of lore and arcana from the Forgotten Realms setting, to allow players to create and equip characters. The book includes races, feats, spells, prestige classes, and magic items for the 3.5 edition update to the setting, and includes material from 1st and 2nd edition.
The water recharges in the West Bank mountains and ends in the springs of the Yarkon River at Antipatris, and Taninim Springs on the coastal plain of the Mediterranean. [ 1 ] The model adding the Beer Sheva region aquifer to the direct sources of the Yarkon springs was laid down by Samuel Mandel in 1961 and has since been contradicted by work ...
Its eastern part consists of sandstone, ending in Karkur Talh. In Karkur Murr, there is a permanent oasis ( Guelta ), called Ain El Brins (Bir Murr). In the sandstone part, four plateaus emerge from the level of the surrounding desert: the Hassanein plateau, connected to an unnamed plateau through a narrow neck, the Italia plateau and another ...
Eoarchean geology is the study of the oldest preserved crustal fragments of Earth during the Eoarchean era from 4.031 to 3.6 billion years ago. Major well-preserved rock units dated to this era are known from three localities, the Isua Greenstone Belt in Southwest Greenland, the Acasta Gneiss in the Slave Craton in Canada, and the Nuvvuagittuq Greenstone Belt in the eastern coast of Hudson Bay ...
The Rheic Ocean had completely disappeared, and the western Paleo-Tethys was closing. By the Late Permian, the small elongated Cimmerian plate (today's crust of Turkey, Iran, Tibet and parts of South-East Asia) broke away from Gondwana (now part of Pangaea). South of the Cimmerian continent a new ocean, the Tethys Ocean, was created.
The western part of the ridge (the Weald of Kent, Sussex and Surrey in England) has been greatly eroded, with the presumed chalk surface removed to expose older, Lower Cretaceous rocks (Wealden Group) and a small area of Upper Jurassic Purbeck Beds. [2]