玄武岩

「玄武岩」的造型概念来自风化后的玄武岩群。玄武岩是一种细粒致密、外观呈黑色的火成岩,由基性岩浆喷发凝结而成。 玄武岩岩浆的黏度小,易于流动,形成很大的覆盖层,常形成广大的熔岩台地,分布很广,形成硕大迷人的视觉景象。没有被风化的玄武岩凝结后产生六方晶体节理,风化后形成六方柱状,正如目前「玄武岩」表面造型设计为连续正六边形所组成的一个陷落曲面,为一个微小而精致的人造景观。
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玄武岩

玄武岩

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玄武岩

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