{{technical|date=December 2014}} {{Infobox fault | name = Ross Lake fault | other_name = Ross Lake fault zone | namedfor = | namedby = [[Peter Misch]]<ref>{{Cite Q| Q61461210|page=46}}</ref> | yeardef = | image = | image_size = | image_alt = | image_caption = | pushpin_map = | pushpin_map_width = | pushpin_map_caption = | pushpin_map_alt = | pushpin_relief = | pushpin_map_label = | pushpin_label_position = | pushpin_mark = | pushpin_mark_size = | location = | country = {{flag|USA}} {{flag|Canada}} | region = [[North America]] | state = | cities = | coordinates = | elevation = | elevation_m = | elevation_ft = | elevation_ref = | topdepth_m = | topdepth_ft = | topdepth_ref = | range = | part_of = | segments = | length = | width = | depth = | strike = | dip = | dip_angle = | displacement = | plate = | status = | earthquakes = | type = | movement = | rockunit = | age = | orogeny = [[Cordillera]] | volcanic_arc/belt = | map_image = | map_caption = | embed = }} The 10 kilometer wide '''Ross Lake fault''' zone (RLFZ) is part of a 500 kilometer long zone of high-angle [[geologic fault|faults]] in the [[North American Cordillera]] of [[Washington (state)|Washington]] and [[Canada]].<ref>{{cite Q| Q97503730|page=662}}</ref> The RLFZ consists of two major sets of faults. The eastern set of the [[Hozameen Range|Hozameen]] and Slate Creek faults and more southerly North Creek fault form the western boundary of the Jurassic-Cretaceous [[Methow River]] basin and in part separate it from metamorphic equivalents of Methow strata. Minor structures along the North Creek fault record dextral [[Fault (geology)#Strike-slip faults|strike-slip]] events that occurred between approximately 88 and 50 [[myr|Ma]]. The same formations lie on both sides of the faults, implying modest slip (tens of km?). The northernmost strand of the western fault set, the Ross Lake fault itself, is a vertical zone of horizontally-lineated [[mylonite]] that separates upper-amphibolite-facies rocks of the [[Cascade Range|Cascades]] crystalline core from sub-greenschist-facies rocks to the east. Some [[Fault (geology)|dextral shear]] and 6–12 km of NE-side down normal slip occurred from 50(?) to post-45 Ma. At Elijah Ridge, the Ross Lake fault steps westward across a gently dipping extensional zone to the [[Gabriel Peak (Washington)|Gabriel Peak]] tectonic belt. This approximately 100 kilometer long, northeast-dipping mylonite zone is dominated by flattening, but kinematic indicators record dextral shear in the north and reverse shear farther south. This transpressional deformation occurred from 65 Ma (and earlier?) to 58 Ma when at least 7–24 km of dextral slip was probably transferred to the eastern faults by ENE-striking shear zones. Younger (< 50 Ma) ENE-striking sinistral faults at least locally accommodated 5–10 km of dextral strike slip by vertical axis rotation. The fault sets merge southward to form the Foggy Dew fault zone where mylonites record oblique dextral-normal slip (down-to-E). Slip is bracketed between 65 and 48 Ma; some occurred after 60 Ma and the zone records the regional transition from approximately 65–58 Ma [[transpression]] to approximately 57–45 Ma transtension. The fault zone is truncated to the SE by the 48 Ma [[Cooper Mountain (Oregon)|Cooper Mountain]] [[batholith]], which also obliterates its intersection with the southern continuation of the Pasayten fault. South of this batholith, only a narrow, discontinuous [[shear zone]] is on strike with the Foggy Dew fault and similar units lie on both sides of this projection of the RLFZ.
==References== {{ref-list}}
[[Category:Geology of North America]] [[Category:Seismic faults of Canada]] [[Category:Seismic faults of the United States]]