NEW GEOLOGIC MAP OF THE NORTHERN ALASKA PENINSULA REGION OF SOUTHWEST ALASKA
Important new interpretations derived as a result of this effort include recognition of 3 distinct geologic domains or provinces that have been joined since at least Cretaceous time, all intruded by 60 to 70 Ma plutons. On the basis of geologic and geophysical data, we have demonstrated that the so-called Mulchatna fault is probably not a fault, although we can not yet explain the cause for the linear along the Mulchatna River. Surficial mapping on the west side of Cook Inlet, east of the Alaska Range shows evidence for rapid uplift and alluviation, resulting in a deltaic features, including natural levees which are rarely recognized in Alaska. In addition, during early Pleistocene time, a major glacial lake system was dammed behind massive glaciers derived from the Alaska Range on the east and the Ahklun Mountains on the west.
We recorded geologic data for this map in a system of spatial and text databases which allow production and analysis of specialized or derivative maps. The data contain brief unit descriptions, the geologic unit assigned from original published sources where previous mapping was available, and the source information. Additional attributes correlate geologic units to adjacent quadrangles and can be linked through related files to labels, colors, lithology, and age for each unit. Other attributes describe the nature of contact relationships between units.