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.‘ e ‘T1,: .’ .1?
2 ;7,( ‘ >;gf :.
3 . kt. ilA('gy'.:‘
:33 ‘X i 58 y MURLOCH pay’.
31 : ‘ A ,3
h ll’ grounds of M‘Neill, Esq., beyond which are theruina
53 . M 1 3 3 ‘g of Castle Carraf‘ from whence to the bay of Murloch, be-
‘P. 5 3‘ ‘ ‘ ( yond the point of Tor, the cliffs of Cushleak consist of mica
A ‘ slate, containing subordinate beds of primitive lime-stone,
i V 5 syenite, and felspar porphyry. The hills behind the cliffs,‘
" . as they approach Murloch bay, become coverediwith
- :r beds of red sand-stone, and chalk towards the summit,
9: . ,1 and some of the highest points exhibit caps of basalt. r
1 i j ' j 1 The point of Tor is about iive miles distant from Cushe
3. ‘, ‘i h ‘ I endun, and is a projection of the cliffs of Cushleak. It is
3:; the nearest point of';1lax1d- to Scotland, being not more
5:: i H. i,‘ 1 than 18 miles from Cantyre. This proximity of countries
: Av , " l,-‘f A was turned to animportant purpose by the Scots, who
5 7 ' . 2 invaded and seized on territoriesin the county of Antrim:
‘l”i '7-i " they used to kindle. great fires upon the point of Tor,‘
F T ] whenever they apprehended danger from the lrish, to
‘ 3 v ‘r . warn their countrymen of its approach; in consequence
7 - r of which Tor point was formerly called “The Scots
.‘ . Warning Fire." Upon the head of Tor are the remains
f I y of an old- building, called Dunavarre, andalso the great '
Em . K ‘r: fort.‘ It is. supposed to- have been erected by giants,
‘; " Z s ” i i whose burying place is shewuat a little distance from the
1 Vii; .;' fort, called Sleachpt-na-Barragh.
fl 1‘ A little beyond. Tor is Murloch bay, from ‘whence the
- 1‘ A basaltic hillssare. visible, wl1ose formationhasjustbeende-
' . . i‘? ii scribed.’ The. promontories, on the north side of the bay,
y p 5 ‘ 2 exhibit cliffs at the base composed of beds of V mica slate,
r‘ ; ’ j .3’; below which are immense lines of rude fragments of pri-
. l “ mitive rock. On the beach is a very remarkable basaltic 1
l; i‘ ‘.1)’k9, rising in a projecting cragui and to the north is the
' , detached conical mountain of Drimnakill, formed by avast
Fl 1 ‘ ll
, ll ‘1 Probably a corruption of Carey.
- , “’. 1-?
l t ‘E5’ ‘
l‘‘”‘“”‘‘‘ ' "."” 1245;.