> Gran Canaria, like most of the Canary Islands, shows evidence for young basaltic volcanism in the form of cinder cones and valley‐hugging lava flows. These l'/> Sacred ground; the Maipés necropolis of north‐west Gran Canaria
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Sacred ground; the Maipés necropolis of north‐west Gran Canaria

机译:神圣的地面; 西北大加那利岛的麦佩斯大墓地

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> Gran Canaria, like most of the Canary Islands, shows evidence for young basaltic volcanism in the form of cinder cones and valley‐hugging lava flows. These landforms were of no particular use to the aboriginal population, nor to the subsequent Spanish settlers, and young lava flows and lava fields are still referred to as ‘ malpaís ’ (badlands) in the Canary Islands. In north‐west Gran Canaria, one such lava flow fills the bottom of a steep‐sided valley, which reaches the sea at the present day village of Agaete. The lava flow erupted c . 3030 ± 90 yr bp and displays a total length of ~ 11 km. At its distal end, just outside Agaete, it hosts one of Europe’s largest and most important pre‐historic burial sites constructed of volcanic rock: the Maipés necropolis. Over 700 pre‐historic tombs (or tumuli) constructed from the aa ‐type clinker materials have been identified on top of the valley‐filling lava flow. The up to soccer‐ball sized vesicular clinker fragments are sufficiently low in density to provide abundant, workable basalt blocks for the construction of the tumuli, allowing the pre‐hispanic aboriginal population to create a large and magnificent ‘sacred ground’ in an otherwise barren landscape.
机译: > 格兰加里亚,如大多数加那利群岛,显示了煤渣锥形式的年轻玄武岩火山主义的证据,拥抱熔岩流动。这些地貌对土着人口没有特别用途,也不是随后的西班牙定居者,幼兰流量和熔岩田仍被称为“ malpaís “(荒地)在加那利群岛。在西北大加那利岛,一个这样的熔岩流填充了一座陡峭的山谷底部,即在当天的agaete村到达海。熔岩流爆发了 c 。 3030±90 yr bp 并显示总长度〜11公里。在其远端,恰好在Agaete之外,它举办了欧洲最大,最重要的历史悠久的墓地之一,由火山岩(火山岩)建造:麦佩斯墓地。超过700个历史历史古墓(或巨大的墓葬) aa 型熟料材料已经在谷灌浆熔岩流上鉴定出来。直到足球 - 球尺寸的囊泡熟料片段的密度足够低,以提供丰富,可行的玄武岩块,用于构建Tumuli,允许前西班牙裔人群在另一个贫瘠的人群中创造一个大而华丽的“神圣的地面”风景。

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  • 来源
    《Geology Today》 |2019年第2期|共8页
  • 作者单位

    Department of Earth Sciences Section for Mineralogy Petrology and Tectonics (MPT)Uppsala UniversityUppsala Sweden;

    Instituto de Estudios Ambientales y Recursos Naturales (i‐UNAT) Universidad de Las Palmas de Gran Canaria (ULPGC)Las Palmas de Gran Canaria Spain;

    Department of Earth Sciences Section for Mineralogy Petrology and Tectonics (MPT)Uppsala UniversityUppsala Sweden;

    Instituto de Estudios Ambientales y Recursos Naturales (i‐UNAT) Universidad de Las Palmas de Gran Canaria (ULPGC)Las Palmas de Gran Canaria Spain;

    Instituto de Estudios Ambientales y Recursos Naturales (i‐UNAT) Universidad de Las Palmas de Gran Canaria (ULPGC)Las Palmas de Gran Canaria Spain;

    Department of Earth Sciences Section for Mineralogy Petrology and Tectonics (MPT)Uppsala UniversityUppsala Sweden;

    Department of Earth Sciences Section for Mineralogy Petrology and Tectonics (MPT)Uppsala UniversityUppsala Sweden;

    Department of Earth Sciences Section for Mineralogy Petrology and Tectonics (MPT)Uppsala UniversityUppsala Sweden;

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  • 正文语种 eng
  • 中图分类 地质学;
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  • 入库时间 2022-08-20 03:12:12

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