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<br /> <br /> <br />SI'/I/i'Il1ho 8. /87/. li/iITIIIIIIII <br /> <br />I :-)g <br /> <br />F()lIRTII SE(;i\IENT <br /> <br />Labyrinth Canyon <br />Camera Stalioll 723 <br /> <br />Following Ikalnan's route, we have <br />now crossed the river and arc on its <br />southwest hank, looking west-llOrth- <br />west lip the Trin-^IcO\T. 0111' exact lo- <br />cation is has cd on the distinctive (CllT- <br />ground rock, 100ver right, and an abut- <br />ment or the C<l1Ivon wall in lhe lower <br />left. <br />The vegelation has changed less than <br />one wOllld expecl. An oak tlTe in the <br />!cJregroulHI or Beaman's piclulT is now <br />dead, but YOllng shoots han' spnlllg <br />lip at its base. l\losl orllw trees on (he <br />(loor or t1l<' canyon arc cot tonwoods, <br />and at least two of' lhe larger ones in <br />lhe IB7I pic(lII'e arc still ali\'('. <br />The canyon is (loured by alluviulIl <br />derived rrotn the Navajo Sandstone, <br />now diss('Cled hv a gllll\' ten f(>et deep. <br />No dissection, howcver, can he seen in <br />lhe Beamall photograph. All (he visible <br />bedrock IS Na\'ajo SallClstone, The <br />Sl;lill (deserl \'arIlish) 011 the right can- <br />\011 wall appears (0 1)(' ;dJOlIl llw S;1I11<' <br />(oda\', ;dthollgh ,S(lIne sl;,ill(,(] rock 111;1\ <br />Ila\'(' spalkd a\\a\'. ^ k\\ lhill \;I\{TS <br />ha\T spalled li'olll the hce or the rock <br />ill lll<' ri,gh( fiJl(',grolIlHI. Nol<' lll<' ripple <br />IlIarks Oil lhis rock \'isilJk ill S(ephens""; <br />piclllre: (h('\ iIHlic;I((' (hc ;I('lioll or,sh;d. <br />10\\ \\'al('l (1I1 IOOSCS;UHh s('(liIIWIIl. a,s <br />Oil lH'acll<'s. <br />