Single parent dating kahuku hawaii

The lake is very small and shallow, with a surface area of 0.73 ha (1.80 acres) and a depth of 3 m (10 ft).

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Hilo Ridge, a prominent underwater rift zone structure east of Mauna Kea, was once believed to be a part of the volcano; however, it is now understood to be a rift zone of Kohala that has been affected by younger Mauna Kea flows.

Until 1993, artesian water was not known to be present in the Island of Hawaii.

Drilling by the University of Hawaii at that time encountered an artesian groundwater aquifer at 300 meters below sea level and 100 meters of hole depth within a compacted layer of soil and lava where the flows of both Mauna Loa and Mauna Kea meet (Humuula saddle region).

Late volcanism has also given it a much rougher appearance than its neighboring volcanoes; contributing factors include the construction of cinder cones, the decentralization of its rift zones, the glaciation on its peak, and the weathering effects of the prevailing trade winds.

Mauna Kea last erupted 6,000 to 4,000 years ago and is now considered dormant.

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