Editing Horst and graben (section)

== Examples ==

* The [[Basin and Range Province]] in the western United States is an extensive region of alternating valleys and ridges caused by horst and graben as well as [[tilted block faulting]].<ref name=":0" />

* The [[Condroz]] and [[Ardennes]] regions of [[Wallonia]] are good examples of a succession of horst and graben.

* The [[Satpura Range]] is a horst in India and is flanked by [[Narmada River|Narmada]] Graben in the north and much smaller but parallel [[Tapti River|Tapi]] Graben in the south.<ref>{{Cite book|url=https://books.google.com/books?id=BtsLCwAAQBAJ&dq=satpura+horst&pg=PA766|title=The Making of India: Geodynamic Evolution|last=Valdiya|first=K. S.|date=2015-11-26|publisher=Springer|isbn=9783319250298|language=en}}</ref><ref>{{Cite book|date=2017-01-01|chapter=Satpura Horst and Narmada–Tapi Grabens|language=en|volume=22|pages=237–247|doi=10.1016/B978-0-444-63971-4.00010-4|issn=0928-2025|title=Neotectonism in the Indian Subcontinent - Landscape Evolution|series=Developments in Earth Surface Processes|last1=Valdiya|first1=K.S.|last2=Sanwal|first2=Jaishri|isbn=9780444639714}}</ref><!-- add more examples, turn into a table -->