!3! 
VI 
XIV 
XLV 
XXXIV 
\ \ \ I 
XVI 
SIX 
XXIX 
XXII 
XXXV 
XXV 
xm 
X V 1 1 
XLII 
Will 
XXXVI 
XXVIII 
Fair Head 
Bally voy and Cnlhame (Ballycastle) 
Killagan and Olarryford . . 
I '.l I I \ 1 1 ICl III 
Kilwaughtcr (Larne) 
Cranllold Point, N. shore, Lough Neagh 
Antrim Gravels, near Antrim Station 
Woodburn Glens, Carrlckfergus 
Greenisland Station 
Qnarry behind Caramoney Church 
Cave Hill (McArt’s Fort) 
Ballyholme, Bangor 
Crumlin and Glenavy, E. shore of Lough Neag 
Wolfhill and Llgoniel, Belfast 
Dlvis Mountain . . 
Black Mountain 
Brickfields round Belfast 
Neill’s Hill 
Mori Ison 's Sand Pit, Dundonnld Station 
Ballyoran and Carrowreagh 
Colin Glen 
Longhurst, Dunmurry 
Island Hill and Rough Island. N -W. shore 
Lough 
Castle Espie 
W. shore of Strangford Lough 
Dungannon 
Dromore 
Armagh 
Tyrone 
Down 
Armagh 
1,300 to 1,4( 
600 
30-220 
Sea level 
39 
Sea level 
Sea level 
90 
100 
Sea level and 
Trias 
Basalt 
Trias 
Carboniferous 
Silurian 
Carboniferous 
Silurian 
s and g 
b e, s and g 
Derived Fossils. 
Cret 
Carb, Lias, Cret 
Cret 
Cret 
Sil, Carb, Lias, Cret 
Cret 
Lias 
Carb (Castle Espie) 
Relative Proportion of 
Shells 
Shells 
For and Ostra 
None 
For (May, 1906) 
For (very rare) 
Abbreviations Types of Drift— Is d— loose, stoney drift ; b c— boulder clay ; s— sand; g— gravel. 
Compass direction In which the parent rock of erratics Ilea, taken from tho localities whore such 
erratics were fouud. 
W.N.W.j 
N.W. 
N, N.W. 
N. 
N.N-E. 1 
1 N.E. 
E.N.E. 
E. 
E.8.E. 
|„ 
S.S E. 
S. 
S.S w. 
s.w, 
W.8.W, 
Ino, 
8 
1 
8 
1 1 
1 J 
1 
'g 
’• 
:: 
3 
*2 
2 
3 
1 
2 
1 
I? 
1 2 1 
7 
12 
1 
8 
2 
18 
*i 
2 
9 
81 
*8 
1 
i 
8 
\l 
; i 
17 
18 
20 
1 
6 
3 
g 
1 
1 :: 
3 
22 
28 
•i 
6 
2 
1 :: 
1 
"i 
26 
20 
2 
1 
1 
27 
'l 
‘3 
2 
- 1 . 
1\ 
29 
*3 
* 
2 
1 
'i 
‘i 
32 
1 :: 
3 
10 
*i 
*2 
84 
1 ■■ 
‘i 
30 
I- 2 1 
14 
26 
os 
10 
47 
3 
2 
11 
8 
14 
1 
2 
Shells.— frag— fragmentary, 
Microzoa.— For-foraminifera ; Ostra— Ostracoda. Blanks indicating that the drifts of that locality have not yet been examined. “ None "—that drifts were examined and none found 
The relative proportion of erratics was ascertained from boulders of all sizes taken at random and counted. 
The Compass direction is only given for erratics, whose parent rock is definitely ascertained, excluding rocks found in situ in more than one locality. 
