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PENANG-MALACCA
J. A. Goetzee, general manager W. Price, assist. manager
C. E. Peglar, branch manager (Ipoh)
T. McGowan,
H. M. Orloff,
G. F. Gray, Assistants-
J. A. Rous R. Jacobs
J. M. Summers
do.
(Taiping)
do. (Teluk Anson) do. (Alor Star)
G. A. Pridmore R. J. Beer
WILSON & Co., LTD., G. W., Merchants-
Church Street; Teleph. 699
R. P. Brash, managing director
B. Somerset
YOUNG & Co., LTD., R., Civil, Construc- tional & Sanitary Engineers, Specialists in Reinforced Concrete- Registered Office: 3, Weld Quay; Office and Show- room: 1, Penang Road; Works: Sungei, Pinang; Quarry and Tileworks: Ayer Itam; Teleph. 542; Tel. Ad: Loco; Codes: A.B.C. 5th and 6th edns., Engineering 2nd ed., Broomhall's Imp., Bentley's ph.
Directors-J. W. Hunt (chairman) and
E. V. C. Thomson
J. W. Hunt
R. F. Brelsford, A.M.I.C.E. C. H. Young
Ipoh Branch
J. C. Williamson
D. C. Edgar, A.R.I.SAN.E., manager
MALACCA
The Settlement of Malacca excites more interest from a historical point of view than either of its sister towns. Commercially, it fell completely to the rear after the establishment of Penang and Singapore, but the advent of the rubber industry in 1906 converted the settlement into a flourishing agricultural province. Originally set- tled by the Portuguese in 1511, it was for many years the one foreign entrepôt in the East, and the fact that it has given its name to the Peninsula and that it was the cradle of Anglo-Chinese study attest its former importance. Its area is embraced by boundaries some 42 miles in length, with a breadth of from eight to 25 miles. It is governed by a Resident Councillor in subordination to Singapore.
The geological formation of the territory of Malacca consists chiefly of granite rocks, overlaid in several places by the red cellular clay iron-stone called by geologists laterito. Many of the low plains are alluvial, the soil composed of decayed vegetable mould interlaced with sand. The metallic ores are iron and a little tin. The surface generally is undulating, consisting of low round ridges and narrow valleys, the only mountain of considerable elevation being the Ophir of the Portuguese, which is just over the border in Johore territory, 4,187 feet above the level of the sea. It is called by the Malays "Gunong Ledang."
The mineral products of Malacca were at one time looked upon as offering valuable prospects. Gold to the extent of 1,500 ounces yearly was obtained in 1857-8, just outside the confines of the present territory, but the yield decreased to such an extent that it is no longer worked. Tin, about the same period, assumed considerable importance. The first mines were opened in 1793, but no great enterprise was displayed until 1848. when some 5,000 cwt. was the annual product. This increased until 1858, and a large number of Chinese were employed in the industry. The superior yield of the Native States, however, combined with the exhaustion of the surface workings, resulted in mining enterprise in Malacca being virtually abandoned. A little tin mining still goes on in the Jasin district, and gold may possibly exist in very small quantities.
The climate of Malacca as to temperature is such as might be expected in a country not much more than 100 miles from the equator, lying along the sea shore-hot and moist. The thermometer in the shade ranges from 72° to 88° Fahrenheit, seldom being so low as the first of these, and not often higher than the last. The range of the barometer is only from 29.8 to 30.3 inches. Notwithstanding constant heat, much moisture, and many swamps, the town at least is remarkable for its salubrity, and, with the exception of the early period of its occupation by the Portuguese, has always enjoyed this reputation.
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