Mount Magth

Mount Magth is a towering edifice of a mountain at the southern end of Lake Gyon. The summit of the mountain is perpetually wreathed in cloud, and the upper parts are said to be in snow every day of the year but one. The snow melts in spring and summer, feeding the floods of the Sefth, Gilph and Tolph rivers. The majority of the mountain consists of sheer bare cliffs of greenstone and black basalt, with only the lower reaches and occasional valleys are covered in vegetation. It is widely believed to have never been climbed.   Natural wonder: the Mirror Cliffs of Magth On the upper northern slope of the mountain is a huge, sheer slope made of enormous white-grey slabs of crystal, some fifty feet in height.  This cliff is half a mile high and three miles wide.  When rising and setting on a clear day, the sun glinting off these crystals can be seen as far away as Mantua or the northern Ischindar Sea.   Like many other mountains, Mount Magth is thought to have been the site of one of the Thousand Towers, and to have formed by a volcano during the Great Sundering.