Rock of ages
| Data(s) |
14/05/2013
14/05/2013
2004
|
|---|---|
| Resumo |
[EN] Granite is emplaced deep in the Earth's crust. It cools and crystallises and is subjected to thermal and magmatic events, and to recurrent stresses. It develops textures or fabrics as well as strain patterns which, as erosion brings the rock mass near the surface, find expression in various fracture sets and systems. |
| Identificador |
http://hdl.handle.net/10553/10101 625749 |
| Idioma(s) |
eng |
| Direitos |
info:eu-repo/semantics/openAccess by-nc-nd |
| Fonte |
<p>Binghamton International Geomorphology Symposium (35º.2004. Kentuky): Weathering and landscape evolution: abstracts, p. 31</p> |
| Palavras-Chave | #250607 Geomorfología |
| Tipo |
info:eu-repo/semantics/conferenceObject |
