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Of minute often scaly crystals of feldspar abounding with microscopical black specks; they are generally compact and laminated; others however of similar composition are cellular and somewhat decomposed. None of these rocks contain large crystals of feldspar or have the harsh fracture peculiar to trachyte. These feldspathic lavas and tuffs are the uppermost or those last erupted; innumerable dikes however and great masses of molten rock have subsequently been injected into them. They converge as they rise towards the central curved ridge of which one point attains the elevation of 2 700 feet. This ridge is the highest land in the island; and it once formed the northern rim of a great crater whence the lavas of this series flowed: from its ruined condition from the southern half having been removed and from the violent dislocation which the whole island has.
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