作为地点和时间的弗吉尼亚大峡谷:跨大西洋和美国地质遗产的焦点

Eric J. Pyle, L. S. Fichter
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摘要

弗吉尼亚大峡谷(GVV)是一个更大的地质构造的一部分,它从美国东北部穿过大西洋中部,一直延伸到东南部。该地区的构造形成代表了近 12 亿年的地质历史,而遗留下来的岩石则记录了巨大的构造变化周期。这些地质遗迹为该地区带来了丰富的美景,随着时间的推移,其肥沃的农业和地质资源吸引了许多人。这篇论文追溯了龙8国际官方网站手机版的地质发展、龙8国际官方网站手机版与数千年来居住在龙8国际官方网站手机版的原住民和欧洲殖民者的关系,以及他们发现的地质资源。虽然从地质遗产的角度来看,龙8国际官方网站手机版的地质资源相对较少,但龙8国际官方网站手机版拥有丰富的遗产,这些遗产说明龙8国际官方网站手机版的资源如何支持每个社会的需求和利益,以及龙8国际官方网站手机版的地质环境在过去 400 年美国历史发展的关键时刻所发挥的作用。 补充材料:https://doi.org/10.6084/m9.figshare.c.7047725
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The Great Valley of Virginia as Place and Time: A Focal Point for Trans-Atlantic and American Geoheritage
The Great Valley of Virginia (GVV) is a section of a much larger geologic structure which spans from the northeastern US through the Mid-Atlantic and to the southeast. While the structural formation of the region represents nearly 1.2 billion years of geologic history, the rocks that remain record vast cycles of tectonic change. The legacy of that geology is a rich and aesthetically attractive region that has drawn many peoples over time to its agricultural fertility and geologic resources. This contribution traces the geologic development of the GVV, the relationship of the GVV to the peoples, both indigenous and European colonizers, that inhabited it over thousands of years, and the geologic resources that they found. Although relatively under-expressed from a geoheritage perspective, the GVV possesses a rich legacy of how its resources supported each society's needs and interests, and the role that the geologic environment of the GVV played at critical moments in the historical development of the US over the last 400 years. Supplementary material at https://doi.org/10.6084/m9.figshare.c.7047725
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