Po Pin Chau
http://dbpedia.org/resource/Po_Pin_Chau an entity of type: SpatialThing
Po Pin Chau (Chinese: 破邊洲) is an island in Hong Kong. Off the eastern coast of the East Dam of the High Island Reservoir, the island is known for its hexagonal columnar jointing. The island was originally a cape connected to the mainland, but eventually broke away from the mainland due to years of erosion. The island is administered by the Sai Kung District and is part of the Hong Kong Geopark and Sai Kung East Country Park. The columnar rock formations on the island were formed after a series of volcanic eruptions in Hong Kong during the Jurassic Era.
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破邊洲（英語：Po Pin Chau）是香港一個島嶼，位於西貢區萬宜水庫東壩對出，以六角石柱的奇觀而著名。 1億多年前的侏羅紀時期，香港發生多次火山爆發，噴出大量熔岩及火山灰。噴至火山口邊的火山灰冷卻後，該處成為切面是六邊形的石柱。結構長約200多米，闊約100米，高約63米。 破邊洲原是由糧船灣伸延入海的一個海岬，但因長年受海浪侵蝕，結果與花山分離成為海蝕柱。
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rdf:langString
Po Pin Chau
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破邊洲
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Po Pin Chau (Chinese: 破邊洲) is an island in Hong Kong. Off the eastern coast of the East Dam of the High Island Reservoir, the island is known for its hexagonal columnar jointing. The island was originally a cape connected to the mainland, but eventually broke away from the mainland due to years of erosion. The island is administered by the Sai Kung District and is part of the Hong Kong Geopark and Sai Kung East Country Park. The columnar rock formations on the island were formed after a series of volcanic eruptions in Hong Kong during the Jurassic Era.
rdf:langString
破邊洲（英語：Po Pin Chau）是香港一個島嶼，位於西貢區萬宜水庫東壩對出，以六角石柱的奇觀而著名。 1億多年前的侏羅紀時期，香港發生多次火山爆發，噴出大量熔岩及火山灰。噴至火山口邊的火山灰冷卻後，該處成為切面是六邊形的石柱。結構長約200多米，闊約100米，高約63米。 破邊洲原是由糧船灣伸延入海的一個海岬，但因長年受海浪侵蝕，結果與花山分離成為海蝕柱。
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