page_title: Mauna Kea
section_title: Native history
hierarchical_section_title: Mauna Kea / Human history / Native history
caption_attribution_description: English: A stone structure, possibly a prehistoric marker or lele (altar), in the saddle between Mauna Loa and Mauna Kea, Hawaii, with Mauna Kea in the background
context_page_description: Mauna Kea is a dormant volcano on the island of Hawaiʻi. Its peak is 4,207.3 m above sea level, making it the highest point in the state of Hawaiʻi. Most of the volcano is underwater, and when measured from its underwater base, Mauna Kea is the tallest mountain in the world, measuring 10,200 m in height. Mauna Kea is about a million years old, and has thus passed the most active shield stage of life hundreds of thousands of years ago. In its current post-shield state, its lava is more viscous, resulting in a steeper profile. Late volcanism has also given it a much rougher appearance than its neighboring volcanoes due to construction of cinder cones, decentralization of its rift zones, glaciation on its peak, and weathering by the prevailing trade winds. Mauna Kea last erupted 6,000 to 4,000 years ago and is now considered dormant. The peak is about 38 m higher than Mauna Loa, its more massive neighbor.
  In Hawaiian religion, the peaks of the island of Hawaiʻi are sacred. An ancient law allowed only high-ranking aliʻi to visit its peak.
context_section_description: The first Ancient Hawaiians to arrive on Hawaiʻi island lived along the shores, where food and water were plentiful. Settlement expanded inland to the Mauna Loa – Mauna Kea region in the 12th and early 13th centuries. Archaeological evidence suggests that these regions were used for hunting, collecting stone material, and possibly for spiritual reasons or for astronomical or navigational observations. The mountain's plentiful forest provided plants and animals for food and raw materials for shelter. Flightless birds that had previously known no predators became a staple food source.
  Early settlement of the Hawaiian islands led to major changes to local ecosystems and many extinctions, particularly amongst bird species. Ancient Hawaiians brought foreign plants and animals, and their arrival was associated with increased rates of erosion.
  The prevailing lowland forest ecosystem was transformed from forest to grassland; some of this change was caused by the use of fire, but the prevailing cause of forest ecosystem collapse and avian extinction on Hawaiʻi appears to have been the introduction of the Polynesian (or Pacific) rat.
  The five volcanoes of Hawaiʻi are revered as sacred mountains; and Mauna Kea's summit, the highest, is the most sacred. For this reason, a kapu (ancient Hawaiian law) restricted visitor rights to high-ranking aliʻi. Hawaiians associated elements of their natural environment with particular deities. In Hawaiian mythology, the summit of Mauna Kea was seen as the "region of the gods", a place where benevolent spirits reside. Poliʻahu, deity of snow, also resides there. "Mauna Kea" is an abbreviation for Mauna a Wākea and means "white mountain," in reference to its seasonally snow-capped summit.
  Around AD 1100, natives established adze quarries high up on Mauna Kea to extract the uniquely dense basalt (generated by the quick cooling of lava flows meeting glacial ice during subglacial eruptions) to make tools. Volcanic glass and gabbro were collected for blades and fishing gear, and māmane wood was preferred for the handles. At peak quarry activity after AD 1400, there were separate facilities for rough and fine cutting; shelters with food, water, and wood to sustain the workers; and workshops creating the finished product.
  Lake Waiau provided drinking water for the workers. Native chiefs would also dip the umbilical cords of newborn babies in its water, to give them the strength of the mountain. Use of the quarry declined between this period and contact with Americans and Europeans. As part of the ritual associated with quarrying, the workers erected shrines to their gods; these and other quarry artifacts remain at the sites, most of which lie within what is now the Mauna Kea Ice Age Reserve.
  This early era was followed by cultural expansion between the 12th and late 18th century. Land was divided into regions designed for the immediate needs of the populace. These ahupuaʻa generally took the form of long strips of land oriented from the mountain summits to the coast. Mauna Kea's summit was encompassed in the ahupuaʻa of Kaʻohe, with part of its eastern slope reaching into the nearby Humuʻula. Principal sources of nutrition for Hawaiians living on the slopes of the volcano came from the māmane–naio forest of its upper slopes, which provided them with vegetation and bird life. Bird species hunted included the ʻuaʻu (Pterodroma sandwichensis), nēnē (Branta sandvicensis), and palila (Loxioides bailleui). The lower koa–ʻōhiʻa forest gave the natives wood for canoes and ornate bird feathers for decoration.
caption: A stone structure or ahu facing Mauna Kea, on Saddle Road between Mauna Kea and Mauna Loa
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