Geological Observations on South America by Charles Darwin
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page 6 of 461 (01%)
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metamorphic schists.--Foliation of intrusive rocks.--Relation of cleavage
and foliation to the lines of tension during metamorphosis. CHAPTER VII.--CENTRAL CHILE:--STRUCTURE OF THE CORDILLERA. Central Chile.--Basal formations of the Cordillera.--Origin of the porphyritic clay-stone conglomerate.--Andesite.--Volcanic rocks.--Section of the Cordillera by the Peuquenes or Portillo Pass.--Great gypseous formation.--Peuquenes line; thickness of strata, fossils of.--Portillo line.--Conglomerate, orthitic granite, mica-schist, volcanic rocks of.-- Concluding remarks on the denudation and elevation of the Portillo line.-- Section by the Cumbre, or Uspallata Pass.--Porphyries.--Gypseous strata.-- Section near the Puente del Inca; fossils of.--Great subsidence.--Intrusive porphyries.--Plain of Uspallata.--Section of the Uspallata chain.-- Structure and nature of the strata.--Silicified vertical trees.--Great subsidence.--Granitic rocks of axis.--Concluding remarks on the Uspallata range; origin subsequent to that of the main Cordillera; two periods of subsidence; comparison with the Portillo chain. CHAPTER VIII.--NORTHERN CHILE.--CONCLUSION. Section from Illapel to Combarbala; gypseous formation with silicified wood.--Panuncillo.--Coquimbo; mines of Arqueros; section up valley; fossils.--Guasco, fossils of.--Copiapo, section up valley; Las Amolanas, silicified wood.--Conglomerates, nature of former land, fossils, thickness of strata, great subsidence.--Valley of Despoblado, fossils, tufaceous deposit, complicated dislocations of.--Relations between ancient orifices of eruption and subsequent axes of injection.--Iquique, Peru, fossils of, |
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