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COVER PHOTOGRAPH CAPTION AND FRONT MATTER

Oblique aerial view of the southern end of Kayak Island, Alaska, a narrow, 32-kilometer-long bedrock island that trends offshore in a southwesterly direction. This is one of the most striking geomorphic features on the classic leading edge rocky coast of southern Alaska. Structurally, this island is located in the Kayak Island zone, a southwest trending structural unit that occurs beyond the western margin of the Yakutat terrane, running parallel to the major thrust fault along the border of the Aleutian trench (Winkler, et al. 1992).