Flat-topped Table Top cinder cone (upper right) lies at the NE tip of the triangular NW extension of Unalaska Island. Table Top and its associated lava apron (center) blanket or fill late-Pleistocene topography. Both Table Top and the Wide Bay cone to the east were considered to be Holocene in age, with the Wide Bay cone (just out of view to the right) being among the youngest in a SW-NE-trending volcanic belt that passes through Makushin volcano to the SW.

Photo by Sam Swanson (University of Alaska Fairbanks, courtesy of Alaska Volcano Observatory).

This image is made available as a Public Domain Work, but proper attribution is appreciated.

Table Top