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A lava tree mold, sometimes erroneously called a lava tree cast, is a hollow lava formation that formed around a tree trunk. They are created when lava flows through an area of trees, coating their exterior. The lava cools just enough to create a solid crust around the trunk, but the tree inside burns away leaving a cavity. Molds of trees may be vertical or horizontal. In many cases, mold formation requires slow moving lava, as well as enough time for the mold to chill.

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  • Lava tree mold (en)
  • 溶岩樹型 (ja)
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  • A lava tree mold, sometimes erroneously called a lava tree cast, is a hollow lava formation that formed around a tree trunk. They are created when lava flows through an area of trees, coating their exterior. The lava cools just enough to create a solid crust around the trunk, but the tree inside burns away leaving a cavity. Molds of trees may be vertical or horizontal. In many cases, mold formation requires slow moving lava, as well as enough time for the mold to chill. (en)
  • 溶岩樹型(ようがんじゅけい)とは、流動する溶岩が樹木を取り囲んだ場合に、その後溶岩が冷えて固まった後に、溶岩に囲まれた樹木の幹の跡が、高温の熱によって焼失し空洞部分を形成する現象によってできた、縦穴や横穴などの洞穴を指す。「溶岩樹形」とも表記される。日本では、富士山北麓や浅間山北麓などで溶岩樹型が見られる。特に富士山の北麓地域には顕著に溶岩樹型が分布する。 (ja)
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  • A lava tree mold, sometimes erroneously called a lava tree cast, is a hollow lava formation that formed around a tree trunk. They are created when lava flows through an area of trees, coating their exterior. The lava cools just enough to create a solid crust around the trunk, but the tree inside burns away leaving a cavity. Molds of trees may be vertical or horizontal. In many cases, mold formation requires slow moving lava, as well as enough time for the mold to chill. (en)
  • 溶岩樹型(ようがんじゅけい)とは、流動する溶岩が樹木を取り囲んだ場合に、その後溶岩が冷えて固まった後に、溶岩に囲まれた樹木の幹の跡が、高温の熱によって焼失し空洞部分を形成する現象によってできた、縦穴や横穴などの洞穴を指す。「溶岩樹形」とも表記される。日本では、富士山北麓や浅間山北麓などで溶岩樹型が見られる。特に富士山の北麓地域には顕著に溶岩樹型が分布する。 (ja)
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