[PAR] [TLE] Kaʻū Desert [SEP] The Kaʻ ū Desert is a leeward desert in the district of Kaʻ ū, the southernmost district on the Big Island of Hawaii, and is made up mostly of dried lava remnants, volcanic ash, sand and gravel.  The desert covers an area of the Kīlauea Volcano along the Southwest rift zone.  The area lacks any vegetation, mainly due to acid rainfall. [PAR] [TLE] Kīlauea [SEP] Kīlauea ( , ; ] ) is a currently active shield volcano in the Hawaiian Islands, and the most active of the five volcanoes that together form the island of Hawaiʻ i.  Located along the southern shore of the island, the volcano is between 300,000 and 600,000 years old and emerged above sea level about 100,000 years ago.  It is the second youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian–Emperor seamount chain.  Because it lacks topographic prominence and its activities historically coincided with those of Mauna Loa, Kīlauea was once thought to be a satellite of its much larger neighbor.  Structurally, Kīlauea has a large, fairly recently formed caldera at its summit and two active rift zones, one extending 125 km east and the other 35 km west, as an active fault of unknown depth moving vertically an average of 2 to per year.
[PAR] [TLE] Kaʻū Desert [ SEP ] The Kaʻ ū Desert is a leeward desert in the district of Kaʻ ū , the southernmost district on the Big Island of Hawaii , and is made up mostly of dried lava remnants , volcanic ash , sand and gravel . The desert covers an area of the Kīlauea Volcano along the Southwest rift zone . The area lacks any vegetation , mainly due to acid rainfall . [PAR] [TLE] Kīlauea [ SEP ] Kīlauea ( , ; ] ) is a currently active shield volcano in the Hawaiian Islands , and the most active of the five volcanoes that together form the island of Hawaiʻ i. Located along the southern shore of the island , the volcano is between 300,000 and 600,000 years old and emerged above sea level about 100,000 years ago . It is the second youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian – Emperor seamount chain . Because it lacks topographic prominence and its activities historically coincided with those of Mauna Loa , Kīlauea was once thought to be a satellite of its much larger neighbor . Structurally , Kīlauea has a large , fairly recently formed caldera at its summit and two active rift zones , one extending 125 km east and the other 35 km west , as an active fault of unknown depth moving vertically an average of 2 to per year .
How old is the currently active shield volcano located in the Kaʻ ū Desert?
How old is the currently active shield volcano located in the Kaʻ ū Desert ?
between 300,000 and 600,000 years
between 300,000 and 600,000 years