
The settlement of Pahala serves as the primary hub for this coastal portion of the Big Island, featuring the Kau High Sch and a local Pahala Landing Strip. The landscape is dominated by volcanic history, most notably the wide Lava Flow of 1823 which stretches toward the Pacific Ocean near Waiwelawela Point. Geologic features like the Great Keaiwa Crack and various Lava Plastered Cones illustrate the area's active terrain, while more remote settlements such as Meyer Camp and Kapapala are situated on the inland slopes.
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