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In tandem with the launch of this expansion, SOE also converted EQ2 into a fully free-to-play MMO. Free players were restricted in what they could access and utilize, while players were able to upgrade to "Silver" level membership for a small one-time fee [15] to get more access. A "Gold" membership cost the same as the existing monthly ...
A render of the new player race, the Sarnak. The Sarnak in EverQuest were an NPC race that inhabited part of Kunark. In Rise of Kunark there are two distinct types of Sarnak: NPC characters who will be familiar to players of the original EverQuest; and the new, playable Sarnak, who were "magically engineered" to fight in the war against the Iksar Empire.
Promotion at E3 2006. SOE markets EverQuest II not as a direct sequel, but as a "parallel universe" to the original EverQuest.It is set in an alternate future of the original game's setting, having diverged at the conclusion of the Planes of Power expansion (the lore is explained in an in-game book).
A phenocryst is an early forming, relatively large and usually conspicuous crystal distinctly larger than the grains of the rock groundmass of an igneous rock. Such rocks that have a distinct difference in the size of the crystals are called porphyries , and the adjective porphyritic is used to describe them.
Phaneritic rock: Anorthosite from the Stillwater Igneous Complex (Neoarchean; Montana) Igneous textures include the rock textures occurring in igneous rocks.Igneous textures are used by geologists in determining the mode of origin of igneous rocks and are used in rock classification.
A similar type of crystal is a phenocryst, a large crystal in an igneous rock. Porphyroblasts are often confused with porphyroclasts, which can also be large outstanding crystals, but which are older than the matrix of the rock [citation needed].
Dacite from the Lassen Volcano National Park. Dacite (/ ˈ d eɪ s aɪ t /) is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides.
Megacrystic porphyroblasts in metasomatised Quartenschiefer (metapelitic unit in the Alps) In geology, a megacryst is a crystal or grain that is considerably larger than the encircling matrix.