76 
gallery and case — or if the ee of the group in the scientific 
sequence adopted in the collection 1s known, or if the number of the 
case in which the nea is situated is known, by looking it up in the 
catalogue. 
The catalogue, when ше: with its guides, сап be used by 
anyone, for there is no elaborate system or set of symbols to learn and 
reme Thi 
r before it can be understood. s elaboration is the great 
k to some of the ingenious systems which n prop 
In my experi m administration, time is always too short 
to do the work which should be done, and th ul innovations are 
those which e time and ню . In this connection 
2 ed, that, as the entries on о t of cards are exact copies of rr 
i f 
m the other set, = cod “capable of copying can do one half o 
e icm work of registra 
[Reprinted from the * Museums Journal," June, 1905.] 
А SHORT ACCOUNT OF SOME *ANCIENT REMAINS" 
FOUND ON GUNONG JERAI, KEDAH 
(WITH ONE PLAN.) 
Br Mg. BR. W. IRBY, 
OF THE PERAK TRIGONOMETRICAL SURVEY, FEBRUARY, 1894. 
(XUNONG JERAL more generally known as Kedah Peak, is a 
the N.N.-E. of Penang. It has a very abrupt and sharp appearance as 
seen from + lr south, but on the northern and western sides it is quite 
easy of as 
The top of Jerai itself is a quartz sandstone, with a dip of about 
15° to the north-west, but cut off on the south by a precipice of 
about 140 feet in height with a strike N. 53° east. Below this эйт 
pice boulders and intrusive granite сап be seen. The crest of Jera 
evidently the result of an upheaval, the centre of action of which wai 
immediately below. The formation, being very е has been 
on the southern slopes and now forms a sca The sand- 
stone on the northern and western slopes is generally uniform in its 
bedding, though there are indications of contortion and local metamor- 
phism. It dips beneath the alluvial soil at the foot of the range 
and passing under the sea comes up again in the Bunting islands. 
On these slopes there are no granitic rocks so far as I ти able to 
ascertain, but all are schistose rocks of sedimentary format 
The usual way to approach Gunong Jerai from "mend is by 
pr 
steamer to Kuala Yen, # small rivulet that rises on its western slopes. 
e shore is so shallow that it is not s игиси җы у о approach even with а 
