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The 'Kaū Desert' is a leeward desert on the Big Island of Hawaii, made up of mostly old worn lava, some sand and gravel. The desert covers an area of the Kilauea Volcano along the Southwest rift zone. The area lacks any vegetation, mainly due to acid rainfall.

Contents

Climate

Leisure and tourism

The 1790 eruption

External links

Climate

Ka'u desert is in the rain shadow of Kilauea volcano and receives very little rain (about 150 mm/yr or 6 inch/yr). Its barrenness also has very much to do with sulfur dioxide escaping the vents in the crater and blowing downwind. Sulfur dioxide combines with water to form sulfuric acid which falls as acid rain which creates a harsh, acidic environment.

Leisure and tourism

The Kaū Desert is popular for walking and hiking tours. You can get to the desert if you follow Highway 11 counterclockwise from Kona to the Volcano, As you traverse the desert, you cross the Great Crack and the Southwest Rift Zone, a major fault zone that looks like a giant groove in the earth, before you reach Kilauea Volcano.

The 1790 eruption

In 1790 occurred one of most devastating explosions in Hawaiian history. The eruption produced accretionary lapilli tuff, which is fine volcanic ash that into forms tiny balls as a result of eruptions that involve water. At that time Chief Keoua was traveling around Kilauea to Ka'u to oppose the dominant chief, Kamehameha. At least 80 Hawaiian warriors suffocated from volcanic ash getting into their lungs. The footprints of these warriors are preserved in the ash.

External links

★ General description of Kaū Desert