106 
BATHYMETRICAL SURVEY OF 
The fact that the area between the 25- and 50-feet contour-lines is 
greater than the area between the shore and the 25 -feet line proves the 
flat-bottomed nature of the basin, as well as the fact that the mean 
depth is fully half the maximum depth. The Loch of Drumellie was 
surveyed on the same day as the Loch of Clunie, June 4, 1903; the 
elevation above the sea was determined by levelling from bench-mark as 
being 146-7 feet. The Ordnance Survey officers found the level of the 
lake-surface to be 147 feet above the sea on September 19, 1899. 
Tem'perature Observations . — Temperature observations taken in the 
deepest part of the loch at 11.30 a.m. gave the following results: — 
Surface ()0°'2 Fahr. 
10 feet 59° 0 ,, 
15 ,, 53° -7 „ 
20 „ 50°-7 „ 
30 ,, 49° 5 „ 
40 „ 49° -2 „ 
58 ,, 48° -7 ,, 
This series shows a range of temperature from surface to bottom of 
ll°-5, the greatest fall being one of 5°-3 between 10 and 15 feet, with 
a further fall of 3° between 15 and 20 feet. Compared with the 
temperatures taken in the Loch of Clunie in the evening of the same 
day, this series shows a much smaller range of temperature, the surface 
temperature being 2° lower and the bottom temperature 1°'5 higher, 
although the difference in depth is only 7 feet ; the position of greatest 
fall in the temperature is nearer the surface in the Loch of Clunie, 
and the amount of fall is greater. 
Rae Loch (see Plate XXX.). — Hae Loch (or Ardblair Loch) lies a 
quarter of a mile to the east of the Loch of Drumellie, into which it 
flows, and about a mile to the west of Blairgowrie. It is surrounded 
by low fields and wooded country, and its shores are all weedy, while the 
western portion of the loch is quite filled with weeds. The water 
formerly stood at a higher level, and frequently flooded the road on the 
north side ; it was consequently lowered about 10 feet by a cutting, 
which has since, however, become choked up. It is under half a mile 
in length, less than one-fifth of a mile in maximum breadth, the mean 
breadth being about one-ninth of a mile, or 25 per cent, of the length. 
Its waters cover an area of about 30 acres, and it drains an area seven 
times greater — an area of over one-third of a square mile. Over 30 
soundings were taken, the maximum depth observed being 16 feet. 
The volume of water is estimated at 8,727,000 cubic feet, and the mean 
depth at 6J feet, or 31 per cent, of the maximum depth. The deeper 
water occurs near the eastern end, off which the slope is steep ; at one 
point a sounding of 10 feet was taken only 20 feet from the shore, giving 
a gradient of 1 in 2. The area of the lake-floor covered by less than 
