Trans. Roy. Soc Edin! 
T i 
SHETLAND ORKNEY~(Hoy) 
UPreh oLo neo 
GANOBTONE with: 
woleante Bie th 
he trese 





Mapetones Shales 
Sirnlatirin di ocortonal 
(evra bale the 
Fees whole pacriny slow: into 
Flagstones he 
ery massive Cen gleomenites 



OF the type tithe 
F ipper Cuithnascynups 
Qnylemenitio unit 
About a0 7% Seri brew 
YORANITE, ONLINE Ae 
Seale of w Jae ny aye Fear 

Vol. XXVIII. Plate k 
To accompany emote by Prat 
Old Kesh Sanckstone of Westone Pres: 
E NORTH OF SCOTLAND . Y 
LD RED SANDSTONE (ol TF Int 
VERTICAL ele eae gy NM he noe, ele Figures at the dortom of ech Section do not include the thickness of the Upper Old Rad Sandstone) : : a 
7 An 14 ¥ we Near i TYNET BURN GAMIRILE 
CAITHNESS TARBAT NESS CULLODEN MOOR GALCANTRAY CAWDOR 
foi feo 
eins eoee 







Sided 
wi 
WICK FLACSTONE ceOouP S000 
THURSO FLAGSTONE GROUP sc00 = 

with banite of 
I Atagstone Shalebec 
Wee centre of Croup. 
Plagpstoves Shitles 
thin Limestonas 
Dv 
Red Sindatenas 
d Alipstonm Shales 
An Limestone 
wu wursen Of 
Siturtchetorin, 
Thicker belied: 
Magstones Shales 
Lurtstoros & thin 
unestonesthe grup 
=} beceonar ret tril 
whaly basinis the 
dortovnt: 
Reet Si 
tulle ret Sheatow 


Brvverattrd Qrogemnarvte 
CALA of tate Agere 
ext Narwisterves etlar 
Af Govagteenarntie harale 
nara (ie, 



wePethion of Knedloan Fish bow. 
cere SSS upper 010 neo sanvsrome Ee 





Raldish grey Vlazpy Senin. 
andl surly Shales with 
exccustenal Koetciattad. Rance 
Pick, scales abundant 




UPPER OL0 RED SANDSTONE 




ScniSTS 





Pisgrtimer Dal, Sandatom at 
souk thin Lirsestoner 
SCHIBTD & IKTAUBIVE 
 scuists s 
e 
 CAYBTALLINE ROCKS. 
yma of a mir 
rs x 
pie 4) SCHISTS & INTRUSIVE 
Kat yellow Sundetones 
© CRYSTALLINE ROCKS 
Se) (xarves Conglamaratis 
SchISTS: 
HORIZONTAL DIAGRAM—SECTION TO EXPLAIN THE DEPOSITION OF THE OLD RED SANDSTONE IN THE NORTH OF SCOTLAND 
ORD OF CAITHNESS SUTORS OF CROMARTY 

OmKNEY (Mey Ae) 

SHETLANO 


a “ee 
rs ee caer ashe 



Horizontal Scale of Si//as 



AHLINC REMI, QUARTZ-AOER, GRANITE ae 

