SJCelajamKcke 
: cnd/aivanD. 
5 £ chnus D 
JiaraiwJ). 
TcmaodvD 
1 P PCHCH 
/Boekany D 
P PANDJANG 
Boulders andqravel, 
covcredwiOi scrubs 
IT/anya/t Soeneja i D. 
Cdak Paooh D 
• U - c / I J I 
quartztu Strike E-’W'.jIrata highly inclined with varqi,xq dip / 
$ .Ltujfceloenc 
In the puddle a/'t he stream and. neas- the tef, bank arc racks c fgreywaekcslatc SbukeE lolfdip ic.Uij^f^ ClausMeu"^'^)!^ 
Thidc lagers of flagstvnc, alternating toilh day slate toy ^ ^ 
Rapids 
r 
ngon f Grcgioacke .state and sandstone Strata intensity folded Strike varyhuMvnv -Vi - _ft\ r /„ £.n] Dip varying 
Thick tanas cfg re yw ache. slate Strike E Mif, (1959) 
fl ... . .. . / . J" / .li P. i nirn ■ 
*9. Thick loners cfgreywackc. state Strike E 2016 (195 
dS^T/tin. laminated etau slate Slake ENE , vertical 
\,. Ql a S* IaU “'^h silky lustre Strike ,VK (1951/ 
J nt (tolled lines indicate the direction, of t/i4strOc*oftfia strata 
• Spot where the. photos weir taken 
(1916) Riyortype C. Honumonbl type ClayslStc On hoik sides of (he river high . smooth. monument.shapedrocks 
S/r E W, dip vertical 
S Djcicat ' ^ ‘ 
River. typo A High Aiffs Average strike of strata E.W. dip from- 75 S. to vertical. 
Rivertypo A Symmetrical type flagstone and. dag slate Average strike of the strata Etef( 
Strata, highly outlined, in inani/ places contorted 
SJYHxran q 
S.Enjocrai^. 
SUaJ T ***** protrude /tom- loth j,dc» into the ruerbeeL Flagstone StrB 10 S , strata folded and highly 
mclintd 
z/ River.typcS. Asymmetrical type flagstone and sandg slate Sb-ike varging font EWE. to SVb\ , dip /i-ont So to SO SB 
Onthe left bank sharp piv/ruding edyef /(-on, the outcrops of the sb-ala. on tl,e right laltkflllt rocks 
*2^ V lag stone Strike £ (If. strata ucarli, vertical 
Doany Gong AS. 7$ 
C Uxuslale with quart i veins Strafu cwlical . sO'ike S /0 S 
JSSeiope 
-c\ -Boulder, island covered with forest 
Ke Icxpc 
/roe rm \ \ t C 
(ISM) / hitt. UirnijuxtccLcf ay slate* StrB 20 N r strata.- vertical^ _YV 
S. MenilH.it Sjdc&n, fJso Ecipids , stronq current 
* ' Elay stone on. both sides. St/xitu vertical, strike E .W. 
1'L- C VL.d 004 1 l L V-\Aa 
( 1 312) Thick. bedded flagstone SlrjE. II' 
«$ Bean JiCemet ■ 
SI. 
911 ati i-i t cci 
cV f 'VCLAyjo . o'k.e. -6 9ed u t o l i u tex \yp\s. 'ex A ci e j> 
1 . n r-t n w 0 
o JJcaTiuvemc 
Is la, id coocroi wide finest The narrow passage betweed the island and tke right bank of Dye river is dry at Luo tide 
(JkV)Sucpcscarpn,cnt,pUeateda,idcontcrtcdgregwack*. slcste. and flagstone Strike about £SE 
S. Kalait, . 
llagslate with quast* veins Strike varging front ESE to E strata, vertic al ■ 7t .. 
Here at the turnings of the rwar many bonlder.banks an i found 
'L l i vx rv 
vivcj jx c l i t 1 ) \2eo,t- JCo &xci*6. t , 
i O . /j oO 
^^^tliy/tly contorted clctyslule . Direction/ of strike inconstant 
h) 
cX-ejo a Leo ted t i| d. <2 t e Lj. f 
\ fl ,Ci, ted clagslnte on both sides Average strike ESE .strata vertical or, tenrh, so 
Clayslatc. Sb ikc AiVlVT, dtp 80 ENE Shop cliffs, fine primeval forest on top 
S.Pakit v '* 
hr~^S K edj any 
^ £ ‘p} RCC,<J 0, ° r ‘& b ' d %h(y contorted clayslatc and nitrite iiUerseeled by p.a.i- veins. Strike , varying from iWV.to ,V, dip vortical (1.993) 
(l99Sjr/usv, bedded clay, sandstoiu. withsnAlvetns ofaclvswus (L Rock. island Strata vertical strike E 20 S. 
Bou/Jcr. island., Tooeivd unthefoiesL P LNSEDAP . j 
Folded day slate, dip varying from TO m.,o80ESE traversed by ym'i, -veins in diffo lit dimetwns, alternating will, thin. be, Ideddeepblue c Iwjdate. genuine drawingslaU . Str E 20 5.(1996/ 
!99l) fine sandstone and da, plate ltiahlj eontortod and twisted toaelher \ \\ niddL of the sb , an, .Da, hgreg qucwtrile eontnuwiy pgrUc, intersected by Jiuu-txaeins. This fcej Utino between.- daits late and. fine sandstone SlrE.W da, 8<N //St/) 
Intersected by ntimeivnsiyolirp veins Str E 105. dip K<0 JVSh \ 9^-0^ ~ ~ ° ^ ° ' 
S ,>l lhc Stl ^ ,L Wt Folded clayslatc, intersected by numerous y uadtvems fl 938) 
(lilt) Clay slate, alternating witJvmenaeeous auartsite E to covered with wood 
9 ?e,,T 9 :z?z: y 
. ^ lamau D. 
S Madoc 
S. Sooty 
&U azcal vi btLj , <x ( ii taev L' 
rd to p/i^q te 4 t(lg (So L’t/t (i 
c i u) e jolted t , 'I'VZxxA- k Pi <^' v^e t 
^ i l (cJi cll tl-LA vtxlecl a tow vx d. 
i 
oPj‘ 
loslo 
S Temacelv 
P BOEKANG 
'//ic tslcuid is formed bif great 
masses of floated trunks of trees, 
over udiirJi graoelancL sand have been. lUposit.d 
<-d Lecx t' 
C licet , 'y\xcut9 Lj. jddzso^acll i j CeAFet co xtxxfctxj 
CD e-itdc i’<rt46't . x4 : ten ii-xinx d.a.L'ect 
t-L LjL If tl 
ie tiv-eid 9 c me ail l xv-cctecL cj to u ixd.. 
