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- Q2474249 subject Q2945795.
- Q2474249 subject Q6582734.
- Q2474249 subject Q7037486.
- Q2474249 abstract "Basin and range topography results from crustal extension (extensional tectonics). As the crust stretches, faults develop to accommodate the extension. For example, in the western United States, this topography is built by a number of normal faults that meet at a basal detachment fault. The basins are down-fallen blocks of crust and the ranges are relatively uplifted blocks, many of which tilt slightly in one direction at their tops due to the motion of their bottoms along the main detachment fault. The normal arrangement in the basin and range system is that each valley (i.e., basin) is bounded on at least one side by one or more normal faults that are oriented along, or sub-parallel to, the range front.".
- Q2474249 thumbnail Basin_range_province.jpg?width=300.
- Q2474249 wikiPageExternalLink glossary.html.
- Q2474249 wikiPageWikiLink Q179842.
- Q2474249 wikiPageWikiLink Q2213536.
- Q2474249 wikiPageWikiLink Q2945795.
- Q2474249 wikiPageWikiLink Q47089.
- Q2474249 wikiPageWikiLink Q5265562.
- Q2474249 wikiPageWikiLink Q6582734.
- Q2474249 wikiPageWikiLink Q7037486.
- Q2474249 wikiPageWikiLink Q7189710.
- Q2474249 wikiPageWikiLink Q810178.
- Q2474249 wikiPageWikiLink Q945014.
- Q2474249 type Thing.
- Q2474249 comment "Basin and range topography results from crustal extension (extensional tectonics). As the crust stretches, faults develop to accommodate the extension. For example, in the western United States, this topography is built by a number of normal faults that meet at a basal detachment fault.".
- Q2474249 label "Basin and range topography".
- Q2474249 differentFrom Q2887180.
- Q2474249 depiction Basin_range_province.jpg.