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The Muralla Pircada - an ancient Andean debris flow retention dam, Santa Rita B archaeological site, Chao Valley, Northern Peru

机译:穆拉拉皮尔卡达(Muralla Pircada)-古代安第斯山脉泥石流拦阻坝,圣鲁塔B考古遗址,北秘鲁潮谷

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摘要

Debris flows caused by El Nino events, earthquakes, and glacial releases have affected northern Peru for centuries. The Muralla Pircada, a northeast-trending, 2.5 km long stone wall east of the Santa Rita B archaeological site (Moche-Chimu) in the Chao Valley, is field evidence that ancient Andeans recognized and, more importantly, attempted to mitigate the effects of debris flows. The Muralla is upstream from the site and is perpendicular to local drainages. It is 1-2 m high, up to 5 m wide, and is comprised of intentionally-placed, well-sorted, well-rounded, 20-30 cm cobbles and boulders from nearby streams. Long axes of the stones are gently inclined and parallel local drainage. Case-and-fill construction was used with smaller cobbles and pebbles used as fill. Pre-Muralla debris flows are indicated by meter-sized, angular boulders that were incorporated in-place into construction of the dam and are now exposed in breeches in the dam. Post-Muralla debris flows in the Chao Valley are indicated by meter-sized, angular boulders that now abut the retention dam.
机译:厄尔尼诺事件,地震和冰川释放造成的泥石流已经影响了秘鲁北部几个世纪。 Muralla Pircada是朝北地区的一个朝圣之地,位于Chao谷的Santa Rita B考古遗址(Moche-Chimu)以东2.5公里,是一堵石墙。泥石流。 Muralla位于该地点的上游,并且垂直于当地排水系统。它的高度为1-2 m,最大宽度为5 m,由故意放置的,分类良好,圆形的20-30 cm鹅卵石和附近溪流的巨石组成。石头的长轴轻轻倾斜,并与局部排水平行。使用“装填”结构,将较小的鹅卵石和小卵石用作填充物。米拉拉前的泥石流由米大小的角砾石表示,这些巨石被原地并入大坝的建设中,现在暴露在大坝的马裤中。潮谷中的穆拉拉河后的泥石流由现在与防洪堤邻接的米大小的角巨石指示。

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