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![The Andes of southern Peru; geographical reconnaissance along the seventy-third meridian. Yale Peruvian Expedition (1911); Physical geography; Geology. PHYSIOGRAPHIC AND GEOLOGIC DEVELOPMENT 243. Fig. 161—Types of deformation north of Lambrama near The Andes of southern Peru; geographical reconnaissance along the seventy-third meridian. Yale Peruvian Expedition (1911); Physical geography; Geology. PHYSIOGRAPHIC AND GEOLOGIC DEVELOPMENT 243. Fig. 161—Types of deformation north of Lambrama near](https://c8.alamy.com/comp/RN6W9R/the-andes-of-southern-peru-geographical-reconnaissance-along-the-seventy-third-meridian-yale-peruvian-expedition-1911-physical-geography-geology-physiographic-and-geologic-development-243-fig-161types-of-deformation-north-of-lambrama-near-sotospampa-a-dark-basaltic-rock-has-invaded-both-granite-gneiss-and-slate-sills-and-dikes-occur-in-great-numbers-the-topographic-depression-in-the-profile-is-the-lambrama-valley-see-the-lambrama-quadrangle-material-nevertheless-it-remains-the-dominating-rock-type-over-the-whole-stretch-of-country-from-huascatay-to-huancarama-in-the-northwe-RN6W9R.jpg)
The Andes of southern Peru; geographical reconnaissance along the seventy-third meridian. Yale Peruvian Expedition (1911); Physical geography; Geology. PHYSIOGRAPHIC AND GEOLOGIC DEVELOPMENT 243. Fig. 161—Types of deformation north of Lambrama near
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