Brothers Fault Zone
The Brothers Fault Zone (BFZ) is the most notable of a set of northwest-trending fault zones including the Eugene–Denio, McLouglin, and Vale zones that dominate the geological structure of most of Oregon. These are also representative of a regional pattern of generally northwest-striking geological features ranging from Walker Lane on the California–Nevada border to the Olympic–Wallowa Lineament in Washington; these are generally associated with the regional extension and faulting of the Basin and Range Province, of which the BFZ is considered the northern boundary.
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Brothers Fault Zone
The Brothers Fault Zone (BFZ) is the most notable of a set of northwest-trending fault zones including the Eugene–Denio, McLouglin, and Vale zones that dominate the geological structure of most of Oregon. These are also representative of a regional pattern of generally northwest-striking geological features ranging from Walker Lane on the California–Nevada border to the Olympic–Wallowa Lineament in Washington; these are generally associated with the regional extension and faulting of the Basin and Range Province, of which the BFZ is considered the northern boundary.
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The Brothers Fault Zone (BFZ) ...... with the Yellowstone Hotspot.
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2.5749504e+5
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8.04672e+4
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Wikipage page ID
26,443,413
Wikipage revision ID
734,521,234
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Major geological structures in ...... mpic–Wallowa Lineament .
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43.81361111111111 -120.60333333333334
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The Brothers Fault Zone (BFZ) ...... sidered the northern boundary.
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Brothers Fault Zone
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4.381361111111111e+1
long
-1.2060333333333333e+2
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Brothers Fault Zone
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