新墨西哥州萨拉多河下游的地质和沉积

Socorro region Pub Date : 1900-01-01 DOI:10.56577/ffc-14.209

G. C. Evans

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引用次数: 1

摘要

萨拉多流域下部的地貌和第三纪地质特征与当地沙丘的历史密切相关。沙丘沿着里约热内卢萨拉多的北岸形成，从河口上游七英里，沿着洛马布兰卡的东侧在南岸。

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Geology and sedimentation along the lower Rio Salado in New Mexico

The geomorphology and Tertiary geology 9f tle lower pirt of ihe Rio Salado drainag,e are closely related to the history of the local sand dunes. Dunes form along the noith bank of the Rio Salado for seven milei upstream from the mouth and on the south bank along the east side of Loma Blanca.

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Socorro region

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