A Formica ant suspends a drop of aphid honeydew between her mandibles (which bristle with 7 or more teeth), as she drinks it. 
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Petroglyphs from Bushmen of South Africa illustrating an early hunt with dogs. Picture used with permission from Pietermaritzberg: University of Natal Press.

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Hot islands

What is the source of the heat and lava on the Big Island of Hawaii? Why do the islands get flatter as you go northwest?  John, Tijeras, New Mexico

Dramatic night view of activity at Pu'u O'o on Kilauea's east rift on June 29, 1983. Individual lava fragments are visible in the spray and molten flows are visible on the flanks of the cone. Pu'u O'o fountains reached more than 300 m; flows from this vent entered Royal Gardens and destroyed 7 dwellings in the month following the date of this photo. By September 1986 this cone, at a height of 250 m, had became the highest volcanic landform built on Hawaii in historic times. Photo credit: G.E. Ulrich, Hawaiian Volcano Observatory, U.S. Geological SurveyA high volcano in Hawaii, getting higher on June 29, 1983. Individual lava fragments are visible in the spray (ten-stories high) and molten flows are visible on the flanks of the cone.  By September 1986 this cone had spewed out enough material to become the highest (820 feet (250 m)) volcanic peak formed on Hawaii in historic times. Photo and text credit: G.E. Ulrich, Hawaiian Volcano Observatory, U.S. Geological Survey

The heat source

"The lava comes from a plume of molten rock that rises from deep within the Earth," says Don Swanson, Scientist-in-Charge, Hawaiian Volcano Observatory.

The Big Island of Hawaii is centered over this plume, called a hot spot.

"As the Pacific plate moves over the hot spot, magma pushes through the oceanic crust and, where it reaches the surface, it [piles up and] forms islands," says Pete Winn, Colorado geologist.

The Big Island of Hawaii was created this way. The source of the hot spot's heat, however, is controversial.

"Probably, it is a combination of heat generated by the accretion that formed Earth, radioactivity within the Earth, self compression of the core of Earth and the dissipation of earth-tide energy," says Don Swanson.

Flatter islands to the northwest

According to Gary A. Smith, Professor of Geology at the University of New Mexico, the smaller lower islands of Hawaii began life centered over the hot spot and grew large as the magma pushed upward. The northwestern drift of the Pacific plate, however, slid the volcanic centers northwest off the stationary hot spot and they became extinct. The volcanoes settled to a lower position on the ocean floor as they coasted northwest, down the bulging hot-spot crust. They became lower still as their weight depressed the ocean crust. Finally, the volcanoes crumbled under pelting rain delivered by the trade winds.

"Eventually, the islands will subside to near sea level and then be planed off by waves," says Smith.

 

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