Relação entre o capeamento pedológico e o substrato rochoso-arenoso no oeste do estado do Rio Grande do Sul
The western part of Rio Grande do Sul, which corresponds to geomorphological sector Cuesta de Haedo, is almost entirely composed by volcanic rocks from the Serra Geral Formation, and by sandy sediments from the upper part of the Paraná basin. Because the landscape of the region is susceptible to ero...
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| Format: | Others |
| Language: | Portuguese |
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Universidade Federal de Santa Maria
2017
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| Online Access: | http://repositorio.ufsm.br/handle/1/3335 |