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澳洲、紐西蘭和南太平洋地區
庫姆班加
新南威爾斯
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澳洲、紐西蘭和南太平洋地區
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庫姆班加飯店
庫姆班加出租度假屋
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庫姆班加
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Hanging Rock is a mamelon, created 6.25 million years ago by stiff magma pouring from a vent and congealing in place. Often thought to be a volcanic plug, it is not. Two other mamelons exist nearby, created in the same period: Camels Hump, to the south on Mount Macedon and, to the east, Crozier's Rocks.[citation needed] All three mamelons are made of solvsbergite, a form of trachyte only found in two or three other places in the world. As Hanging Rock's magma cooled and contracted it split into rough columns. These weathered over time into the many pinnacles that can be seen today Hanging Rock contains numerous distinctive rock formations, including the "Hanging Rock" itself (a boulder suspended between other boulders, under which is the main entrance path), the Colonnade, the Eagle and the UFO. The highest point on Hanging Rock is 718 metres above sea level and 105 metres above the plain below.
Hanging Rock is a mamelon, created 6.25 million years ago by stiff magma pouring from a vent and congealing in place. Often thought to be a volcanic plug, it is not. Two other mamelons exist nearby, created in the same period: Camels Hump, to the south on Mount Macedon and, to the east, Crozier's Rocks.[citation needed] All three mamelons are made of solvsbergite, a form of trachyte only found in two or three other places in the world. As Hanging Rock's magma cooled and contracted it split into rough columns. These weathered over time into the many pinnacles that can be seen today Hanging Rock contains numerous distinctive rock formations, including the "Hanging Rock" itself (a boulder suspended between other boulders, under which is the main entrance path), the Colonnade, the Eagle and the UFO. The highest point on Hanging Rock is 718 metres above sea level and 105 metres above the plain below.
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