A basalt fan structure is a basalt formation composed of columnar jointed basalt columns that have slumped into a fan shape. They are most likely created when basalt lava is intruded into a soft material, such as loose volcanic ash, which is unable to support the intrusion. As the basalt cools and forms columns, the ash collapses, causing the lava spread and form a fan shape. The formations can be vertical or any degree of horizontal.
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| - Basalt fan structure (en)
- 玄武岩扇形構造 (zh)
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| - A basalt fan structure is a basalt formation composed of columnar jointed basalt columns that have slumped into a fan shape. They are most likely created when basalt lava is intruded into a soft material, such as loose volcanic ash, which is unable to support the intrusion. As the basalt cools and forms columns, the ash collapses, causing the lava spread and form a fan shape. The formations can be vertical or any degree of horizontal. (en)
- 玄武岩扇形構造(英語:Basalt fan structure)是由柱狀節理玄武岩坍塌成扇形組成的玄武岩地表。當玄武岩熔岩侵入到底表,冷卻后形成柱狀節理時,若圍岩是鬆散的地層或土壤,例如火山灰等,因爲缺乏支撐力。導致柱狀節理玄武岩坍塌成扇形狀分佈。 隨著玄武岩冷卻並形成柱狀,灰燼坍塌,導致熔岩擴散並形成。坍塌形狀不一,有時近垂直狀,或任何角度的水平狀。 玄武岩是一種细粒致密、黑色的火成岩,由基性岩漿噴發凝結而成,主要成分是硅铝酸钠或硅铝酸钙,二氧化硅的含量大约是45-52%,还含有较高的氧化铁和氧化镁 。玄武岩屬火山岩一種,由岩漿侵入到地表,冷卻而形成的火成岩。同一種岩漿,但在地球不同深処冷卻而形成的浅成岩是辉绿岩(粗玄岩),深成岩是辉长岩。 柱狀節理是一種地質結構,由一組緊密相交的的節理面,而形成的有規則的多邊形棱柱或柱陣列。最常見的柱狀節理是在火成岩,是由於火成岩冷卻和收縮而形成的。 在淺成火成岩偶爾也有柱狀節理, 例如熔岩流及凝灰岩都有。柱子的直徑從 3 米到幾厘米不等,最高可達 30 米。柱子的邊數可以從 3 到 8 不等,其中 6 邊是最常見的。 (zh)
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| - A basalt fan structure is a basalt formation composed of columnar jointed basalt columns that have slumped into a fan shape. They are most likely created when basalt lava is intruded into a soft material, such as loose volcanic ash, which is unable to support the intrusion. As the basalt cools and forms columns, the ash collapses, causing the lava spread and form a fan shape. The formations can be vertical or any degree of horizontal. (en)
- 玄武岩扇形構造(英語:Basalt fan structure)是由柱狀節理玄武岩坍塌成扇形組成的玄武岩地表。當玄武岩熔岩侵入到底表,冷卻后形成柱狀節理時,若圍岩是鬆散的地層或土壤,例如火山灰等,因爲缺乏支撐力。導致柱狀節理玄武岩坍塌成扇形狀分佈。 隨著玄武岩冷卻並形成柱狀,灰燼坍塌,導致熔岩擴散並形成。坍塌形狀不一,有時近垂直狀,或任何角度的水平狀。 玄武岩是一種细粒致密、黑色的火成岩,由基性岩漿噴發凝結而成,主要成分是硅铝酸钠或硅铝酸钙,二氧化硅的含量大约是45-52%,还含有较高的氧化铁和氧化镁 。玄武岩屬火山岩一種,由岩漿侵入到地表,冷卻而形成的火成岩。同一種岩漿,但在地球不同深処冷卻而形成的浅成岩是辉绿岩(粗玄岩),深成岩是辉长岩。 柱狀節理是一種地質結構,由一組緊密相交的的節理面,而形成的有規則的多邊形棱柱或柱陣列。最常見的柱狀節理是在火成岩,是由於火成岩冷卻和收縮而形成的。 在淺成火成岩偶爾也有柱狀節理, 例如熔岩流及凝灰岩都有。柱子的直徑從 3 米到幾厘米不等,最高可達 30 米。柱子的邊數可以從 3 到 8 不等,其中 6 邊是最常見的。 (zh)
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