Brothers Fault Zone
The Brothers Fault Zone (BFZ) is the most notable of a set of northwest-trending fault zones including the Eugene–Denio, McLoughlin, 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.
Wikipage disambiguates
Link from a Wikipage to another Wikipage
primaryTopic
Brothers Fault Zone
The Brothers Fault Zone (BFZ) is the most notable of a set of northwest-trending fault zones including the Eugene–Denio, McLoughlin, 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.
has abstract
The Brothers Fault Zone (BFZ) ...... with the Yellowstone Hotspot.
@en
Link from a Wikipage to an external page
Wikipage page ID
26,443,413
page length (characters) of wiki page
Wikipage revision ID
1,021,645,683
Link from a Wikipage to another Wikipage
country
image caption
Major geological structures in ...... mpic–Wallowa Lineament .
@en
length
SE–NW
@en
Location
Between Steens Mountain and Newberry Volcano , approximately
@en
name
Brothers Fault Zone
@en
state
width
SW–NE
@en
wikiPageUsesTemplate
point
43.81361111111111 -120.60333333333334
type
comment
The Brothers Fault Zone (BFZ) ...... sidered the northern boundary.
@en
label
Brothers Fault Zone
@en
lat
4.381361111111111e+1
long
-1.2060333333333333e+2