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  2. River anticline - Wikipedia

    en.wikipedia.org/wiki/River_anticline

    River anticlines form when huge amounts of material are removed by river erosion in an area with low crustal rigidity. The crust rebounds up specifically along the river, while the rest of the area remains relatively constant. This will bend the crust forming an anticline, which can take up to ten thousand years. [7]

  3. Anticline - Wikipedia

    en.wikipedia.org/wiki/Anticline

    All anticlines and synclines have some degree of plunge. Periclinal folds are a type of anticlines that have a well-defined, but curved hinge line and are doubly plunging and thus elongate domes. [5] Model of anticline. Oldest beds are in the center and youngest on the outside. The axial plane intersects the center angle of bend.

  4. River anticlines - Wikipedia

    en.wikipedia.org/?title=River_anticlines&redirect=no

    What links here; Related changes; Upload file; Special pages; Permanent link; Page information; Cite this page; Get shortened URL; Download QR code

  5. Category:Anticlines - Wikipedia

    en.wikipedia.org/wiki/Category:Anticlines

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  6. Wallula Gap - Wikipedia

    en.wikipedia.org/wiki/Wallula_Gap

    Columbia River Basin. Wallula Gap (/ w ə ˈ l uː l ə /) is a large water gap of the Columbia River in the Northwestern United States, in Southeastern Washington.It cuts through the Horse Heaven Hills basalt anticlines in the Columbia River Basin, just south of the confluence of the Walla Walla and Columbia rivers.

  7. Umtanum Ridge Water Gap - Wikipedia

    en.wikipedia.org/wiki/Umtanum_Ridge_Water_Gap

    The landmark is characterized by a series of steep-sided ridges in the Columbia River basalt which are cut through axially by the Yakima River. A water gap was cut by the Yakima River through anticlines named "Manastash Ridge" and "Umtanum Ridge". These anticlines are part of the Yakima Fold Belt near the western edge of the Columbia River Plateau.

  8. File:River anticline by, Michael Stevens.pdf - Wikipedia

    en.wikipedia.org/wiki/File:River_anticline_by...

    Formation of a river anticline by river erosion and the associated isostatic rebound. As the river erodes the overlying material, the underlying rocks will rebound up, like a block in water if you remove a weight from on top of it, forming an antiformal structure. (Image created by Michael Stevens)

  9. Yakima Fold Belt - Wikipedia

    en.wikipedia.org/wiki/Yakima_Fold_Belt

    Shaded-relief map showing ridges of the Yakima Fold Belt of south-central Washington, mostly between Interstate 90 (red line) and the Columbia River (bottom). Red square in center is the city of Yakima, red rectangle at lower right is the Tri-Cities, red circles are various cities, triangles are the Mount Rainier, Mount St. Helens, and Mount Adams volcanoes of the Southern Washington Cascades.