DescriptionSouthern Washington Cascades conductor.png
English: The Southern Washington Cascades Conductor (SWCC, yellow) located at depth approximately between Mount Saint Helens (MSH), Mount Adams (MA), Goat Rocks (GR), Mount Rainier (MR), and Riffe Lake, with a lobe extending towards Tiger Mountain (TM). MSH and MR are associated with bends and offsets in the seismically active Saint Helens Zone (SHZ) and Western Rainier Zone (WRZ)(thick dashed lines); these bends align with other volcanic features and with a fault at Glacier Peak (GP). The southern portions of the SHZ and WRZ are parallel with a regional orientation of faulting (including the Entiat Fault and Portland Hills fault zone). The w:Straight Creek Fault (inactive) shows 90 km of mid-Eocene right-lateral offset; its southern continuation is unknown. Line "B" marks a boundary in seismic activity.
Also shown: Southern Whidbey Island Fault, Rattlesnake Mountain Fault Zone, w:Olympic-Wallowa Lineament (OWL), White River/Naches River fault, Rimrock Lake Inlier (outlined in green), surface outcrops of the Crescent Formation (outlined in brown), and the Olympia Structure (suspected fault, aseismic). Red square is the White River altered area.
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{{Information |Description ={{en|1=The Southern Washington Cascades Conductor (SWCC, yellow) located at depth approximately between Mount Saint Helens (MSH), Mount Adams (MA), Goat Rocks (GR), Mount Rainier (MR), and Riffe Lake, with a lobe extending t
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