The Saddle Mountains consists of an upfolded anticline ridge of basalt in Grant County of central Washington state. The ridge, reaching to 2,700 feet, terminates in the east south of Othello, Washington near the foot of the Drumheller Channels. It continues to the west where it is broken at Sentinel Gap (a water gap through which the Columbia River passes) before ending in the foothills of the Cascade Mountains.
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| - Saddle Mountains (de)
- Saddle Mountains (en)
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| - Die Saddle Mountains bestehen aus einem aufgefalteten antiklinalen Basalt-Grat im Grant County im zentralen Teil des US-Bundesstaates Washington. Der Hauptgrat erreicht maximal 803 Meter Höhe und endet im Osten südlich von Othello nahe dem Fuß der Drumheller Channels. Er setzt sich nach Westen fort, wo er durch die (eine vom Columbia River durchflossene Lücke) unterbrochen wird, bevor er in den Ausläufern der Kaskadenkette endet. (de)
- The Saddle Mountains consists of an upfolded anticline ridge of basalt in Grant County of central Washington state. The ridge, reaching to 2,700 feet, terminates in the east south of Othello, Washington near the foot of the Drumheller Channels. It continues to the west where it is broken at Sentinel Gap (a water gap through which the Columbia River passes) before ending in the foothills of the Cascade Mountains. (en)
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| - Saddle-mountains.JPG (en)
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| - The Saddle Mountains as seen from the south in the summer of 2006. Note gas drilling rig in the foreground. (en)
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| - 46.806666666666665 -119.55777777777777
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| - Die Saddle Mountains bestehen aus einem aufgefalteten antiklinalen Basalt-Grat im Grant County im zentralen Teil des US-Bundesstaates Washington. Der Hauptgrat erreicht maximal 803 Meter Höhe und endet im Osten südlich von Othello nahe dem Fuß der Drumheller Channels. Er setzt sich nach Westen fort, wo er durch die (eine vom Columbia River durchflossene Lücke) unterbrochen wird, bevor er in den Ausläufern der Kaskadenkette endet. (de)
- The Saddle Mountains consists of an upfolded anticline ridge of basalt in Grant County of central Washington state. The ridge, reaching to 2,700 feet, terminates in the east south of Othello, Washington near the foot of the Drumheller Channels. It continues to the west where it is broken at Sentinel Gap (a water gap through which the Columbia River passes) before ending in the foothills of the Cascade Mountains. (en)
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| - POINT(-119.55777740479 46.806667327881)
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