Laserfiche WebLink
• <br />�' A <br />Yews Bebre <br />I'll, �" 13 <br />, ' <br />DESCRIPTION <br />Geob* Time Scale <br />Al tiw <br />Symbol <br />ON LAND OFFSHORE <br />MAP SYMBOLS <br />Mouof <br />Triangle - termination point data. <br />Historic <br />Displacement during historic time (e.g. San Andreas fault 1906). <br />D Square - lault creep slippage. <br />z <br />Includes areas of known tault creep. <br />�r'� vl <br />, <br />i � <br />' I ��,� <br />\ <br />Vis? <br />�• �'e <br />"� -�,:�. <br />1 t.s� fp �� �",,' <br />�� <br />� <br />���i` <br />,,,s a.,, <br />•� <br />T�.' �' � <br />��r <br />Fault offsets seafloor <br />sediments or strata of <br />ting . i - <br />fro <br />d� <br />s ,&�� <br />� <br />hR�, (F ♦ <br />—i '--- <br />' , I <br />�C�4� �„ .. <br />i . lt. aFM1' �. „� <br />Holocene ace. <br />n <br />�., <br />w. <br />e <br />rz <br />.., <br />t ! . <br />Faults showing evidence of displacement <br />Fault cuts strata of Late <br />_ _ <br />�y <br />• <br />f r <br />s <br />� <br />� <br />Undivided Quaternary faults -most faults in <br />Arrows along fault indicate relative or <br />Z' <br />700.000 <br />I <br />this category showevitlence of <br />apparent direction of lateral movement <br />?' <br />R`n <br />Al <br />Fault cuts strata of <br />P <br />`m <br />a <br />e <br />years; possible exceptions are faults which <br />v ' /j <br />. <br />v <br />7 <br />p' <br />t <br />displace rocks of undifferentiated Plio• <br />Pleistocene age. <br />Low angle fault (barbs on upper plate) <br />Numbers refer to annotations listed in <br />Pre- <br />Ak <br />Faults without recognized Quaternary <br />displacement or showing evidence of no <br />Fault cuts strata of <br />uatemary <br />' <br />ai��q� <br />c a <br />-.f <br />Pliocene or older age. <br />explanatory text of map. <br />t, <br />�. {•t' <br />,�., <br />necessarily inactive <br />171 <br />i " <br />a� <br />x. <br />4 <br />r <br />`W <br />A <br />W�-Ot <br />0, <br />72 <br />r . <br />xstd' <br />i <br />'e6" <br />v <br />t, .P - <br />.r <br />•S. n*jr Ai�'^ ! <br />1 ! y. � <br />� � i^�:" 11�s�g'a �L ..' <br />� <br />Reference: Excerpt of Jennings, C. W, and Bryant, W.A., 2010, Fault <br />activity map of California: California Geological Survey, Data Map <br />No. 6, map scale 1:750,000. <br />Used by permission from California Geological Survey. <br />0 10 20 30 40 50 <br />SCALE IN MILES <br />FIGURE 3 <br />' IAge of Ea fi) JGF INOV 2013 1 2013.A135 <br />Yews Bebre <br />Fault <br />i <br />DESCRIPTION <br />Geob* Time Scale <br />Present <br />Symbol <br />ON LAND OFFSHORE <br />MAP SYMBOLS <br />Mouof <br />Triangle - termination point data. <br />Historic <br />Displacement during historic time (e.g. San Andreas fault 1906). <br />D Square - lault creep slippage. <br />z <br />Includes areas of known tault creep. <br />Hachure -linear extent of fault creep <br />® <br />■ other symbols - see below <br />'8 <br />Holocene <br />200 <br />Displacement during Holocene time. <br />Fault offsets seafloor <br />sediments or strata of <br />Approximately located [race <br />m <br />' , I <br />Holocene ace. <br />--- <br />c <br />Location uncertain <br />11 700 <br />' I <br />Faults showing evidence of displacement <br />Fault cuts strata of Late <br />_ _ <br />during late Quaternary time. <br />Pleistocene age. <br />Bar and ball on downthrown side <br />Undivided Quaternary faults -most faults in <br />Arrows along fault indicate relative or <br />Z' <br />700.000 <br />I <br />this category showevitlence of <br />apparent direction of lateral movement <br />?' <br />displacement during the last 1,600,000 <br />Fault cuts strata of <br />P <br />`m <br />a <br />years; possible exceptions are faults which <br />Quaternary age. <br />Direction of fault dip <br />p' <br />displace rocks of undifferentiated Plio• <br />Pleistocene age. <br />Low angle fault (barbs on upper plate) <br />Numbers refer to annotations listed in <br />Pre- <br />1.600.000 <br />Faults without recognized Quaternary <br />displacement or showing evidence of no <br />Fault cuts strata of <br />uatemary <br />displacement during Quaternary time. Not <br />Pliocene or older age. <br />explanatory text of map. <br />— <br />necessarily inactive <br />171 <br />FIGURE 3 <br />' IAge of Ea fi) JGF INOV 2013 1 2013.A135 <br />