e

Fiq 4. Section t),roue,h Co rick Hill. Pour is h o/‘ Pun given..

Ft q Z. Section through. Praia - na - shoke Mountain.

Craiq nasheke f&oc

PI-ate E.

Fiq. 6. Section on the. Moyoict .River . .Pctri.sh, of Bctllynctscreen..

X ,

Traces „f 0 /, af.^

Potk.LLi.tLr j idenes

*;

Carbon

F.LJ ‘cZF.cUs ch. fi,.. -

Sh

so.*-"

‘r-JX-

bc nX

l r ** -r

V

htaPUl

■ -‘ZZpSz f" 1 ^' ^ 4

"TT

^tp, ,. r M *r/ f

OT cL Red. C or *

C a- r b o

f e. 5s

^ r o i 4 s

trees

0 l tlRed

C a r h c u i r e r o u s S • r i r

-J

f-TZl

LINE OF

SECTION

LINE OF

S E C T I ON

• ^4* l ~t t

.SECTION

46Z& Slteve Galleon Cot

SECT] ON

M/cvt Gg.lti ori . Ca.ru tSZS

bcq. 3. Section, sh£.vn.-nM tiee. relative position, of the cietahheoL BolsoCUic cup of Clteve (tOZLCcTL CctriV.

Fl Cf. 7. Section, sh-ewCnc? Lite position, of the. jLlTTlCStOJlf, cot CwLHoft'.

^C/uUk

r5S =— e " ***** ^taidstone

Shale s and. SccncLstort.es a2>ovjc.th

wir::5^

■Jj/.CLPfi / \ :'V

liff",, 'vV i

4#

\

Light Colouredt-i 'Sandstone

y \ V

Carbon f ShjL.i

V \‘ 'vx^r <ffewHed Sf.

FFK,

-r-~OtC.

Cong/^mer-,

-v-

f 'hi v.-- ■• rff.l . •' ■-

-/ ■

zi :

■/. yplCCr J

i^4

/'/ y ^ /' v ft - ^

if mo- isoommm oofoor,;. iSOfPM ; 'PS'-'OSi n -y-m PfOMOOQ ,;

Old, Red CoTvcfloTnercLte

^s fOirvMsttrct <rb Jiescrcmxrhcn

only rises to about 1.2 feet nsskrum. above ly « * and dipseelaerrit} to this secCttm. ■ «•

M e -t a. m. o r

Wiltl J-fj 1

H o > c k s

\'Or

-*te

‘ftzr

Greenstone

Met am

Fiq. 8. Section on the White Water. Parish of Ballynaserren

LINE OF

SECTION,

LINE

° F Of:

S E C T I ON

■Vf.ieve GitLlicn )130

Fiq. 4-. Section from. Sleeve Gcilttcn, Ca.rn. joomny Fig. 5.

■ v ™ Srt.r*

Fig. 5. Section through SUeve Gcdii on. joimno Fig 4-.

in OO Oh ., \: ;•

From, b to c Rocks are Schistose

s S

V l d It e d J* and s t o ri e

.j • • '>// ' r ;.. C i • ; JJ •;

Oi\ :,L- :/F gif' ; <jj i , \Ol ,X : ■ Vf

'■ocis Prom, a-tv b svmxLa,r to the _*p**T‘i i ' !/ / // ■ ‘l ■ i ' ffl it, ' ' j . < , ■, ,

f ctamorphic Sandstones along {■-' li i V ,l ■ ’/ f • -j. '{I'f'i'&f-' 't\ , i ' ' / / li r fjf '•) , ht ;

U*u of junc tion. ^ ‘ / ' ‘ / V ' • { I <'\ V ; ' A'V ' / / / ^ V ‘ ' 1 ' •/' ■ 1/1 >

■'"''..

rmn if I/.

G r a n i t t f o

fn/m a -to b simU-ccr to Metexmorphny Sandstones alo ng jiu ietLon^.^ '

•li

Prom, c -to d Similar to (he C — „ , , . , i / i, . > I /1 / ■ r . . ■'. \ 'i ;. v-. ' 1. t ,, W/; " /y . J '//.

Jh,r« dto ^JUcT^- ^ areje^rt,^ d Metonjwrphir Sandstones^ ' ‘j' ' j ^Ij' j‘ ’ -/^ // Tf*-' • v \ fa jp / /

rnmf&mpF ■, ■ ■ ■ '“■j

<;/•'• WlMf.* *•• '■M i iSfjrd x .r i-r 1 FM if r- ' /i a , H&f?

Old, Red CffnalomercUf

CarborviferoiLs Series consxs'iaig of a succession, of intcrstrcutificd Shades

*?" impure Limestones. Grits and. course Ctmolmirrixles the Shades heevina Efodicla, Dvthvrocaris. ie

■■■■ '■ ■ f q

j J f i ■;

Fiq. 3. Section wma the succession, of the strata, ut Pm hit lit

./)

ry'P s. sry'v £1$

i*

,.< &s>V’‘

:R. o c k s

o c c -ci s i o it a,-

H o

b l e rv (L i c

G r a 7 i i t i. /’

Rocks

c c a. siona.ll y

Born blond

f r t

Scale., Sur inches to one Mile

UJ 4l\h

Mudtao** t ', :rt*j