page_title: Republic Graben
hierarchical_section_title: Republic Graben
caption_attribution_description: English: Republic Graben, Washington
context_page_description: The Republic Graben, named after the town of Republic, Washington, is one of a number of Eocene extensional basins in what is now the Okanogan Highlands. Having been down dropped it preserves a thick section of volcanic and minor volcaniclastic rocks as well as fossiliferous lacustrine deposits. The volcanic rocks represent the eruptive cover of the widespread Eocene granitic intrusions in the region, and formerly must have been much more widespread.
  Base and precious metal deposits are widespread in the graben.
  The graben projects to the south-southwest under the Miocene basalts in the Columbia Plateau.
  The Early Tertiary-Middle Tertiary graben is 4–10 miles wide and 52 miles long, bounded on the northwest by the Scatter Creek Fault and Bacon Creek Fault, and bounded on the southwest by the Sherman Fault. The middle of the graben is at least 7,000 feet lower than the surrounding blocks. Eocene-Oligocene rocks which formed as the graben subsided include intrusive porphyry and rhyodacite volcanic flows, with some tuff and breccia.
context_section_description: The Republic Graben, named after the town of Republic, Washington, is one of a number of Eocene extensional basins in what is now the Okanogan Highlands. Having been down dropped it preserves a thick section of volcanic and minor volcaniclastic rocks (Sanpoil Volcanics, mainly rhyodacite) as well as fossiliferous lacustrine deposits. The volcanic rocks represent the eruptive cover of the widespread Eocene granitic intrusions in the region, and formerly must have been much more widespread.
  Base and precious metal deposits are widespread in the graben.
  The graben projects to the south-southwest under the Miocene basalts in the Columbia Plateau.
  The Early Tertiary-Middle Tertiary graben is 4–10 miles (6.4–16.1 km) wide and 52 miles (84 km) long, bounded on the northwest by the Scatter Creek Fault and Bacon Creek Fault, and bounded on the southwest by the Sherman Fault.  The middle of the graben is at least 7,000 feet (2,100 m) lower than the surrounding blocks.  Eocene-Oligocene rocks which formed as the graben subsided include intrusive porphyry and rhyodacite volcanic flows, with some tuff and breccia.  The oldest Tertiary formation in the graben is the O'Brien Creek Formation, which is up to 4,200 feet (1,300 m) thick, and composed tuffaceous rock with volcanic ash and rounded quartz grains.  The top of this formation is characterized by an igneous-cemented conglomerate, conformably overlain by the Sanpoil Volcanics, which are about 4,000 feet (1,200 m) thick.  Correlated with these volcanics is the Scatter Creek Rhyodacite, which is generally found along the fault zones defining the graben.  Eocene and Oligocene ore deposits are found within the Republic mining district.
caption: Republic Graben geologic map, Washington
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