From a view-point on western hill-top
Photo: A. Kurata
A. LOCATION
Scotland, UK.
56:57N, 5:45W; 10.1 m above sea level.
B. DESCRIPTION
Of glacial origin, Loch Morar is the deepest lake
in the British isles with a maximum depth of 310.0 m and ranks seventeenth
deepest in the world. It is elongate in shape with its main axis running
in an east-west direction. It has a total length of 18.8 km, a mean depth
of 86.6 m and a volume of 2.3073 km3. Though there are two basins both
deeper than 270 m, Loch Morar is essentially a single large basin, with,
in most places, very steeply shelving sides.
Like Loch Shiel, Loch Morar has moderate watershed
altitude, but very steep slope, very little arable ground and base-poor
geology. But in this lake, there is much less forest around the lake than
Loch Shiel.
The mild winters and cool summers experienced
close to the lake are caused by the damping of seasonal fluctuations in
air temperature not only by the proximity of the Atlantic Ocean but also
by the heat absorption and release of the large volume of water in the
lake itself. Significantly ice is limited to shallow areas, even in severe
winters.
Loch Morar, with the smallest catchment among
the other four Scotland lakes (Loch Ness, Loch Shiel, Loch Awe and Loch
Lomond) drains relatively small area (less than one tenth of that of Loch
Ness). The lake, therefore, is likely to be very nutrient poor (1, 2, 4,
10).
C. PHYSICAL DIMENSIONS (1, 2)
Surface area [km2]
27
Volume [km3]
2.3
Maximum depth [m]
310
Mean depth [m]
86.6
Water level
Regulated
Length of shoreline [km]
60.0
Residence time [yr]
6.9
Catchment area [km2]
142
D. PHYSIOGRAPHIC FEATURES
D1 GEOGRAPHICAL (2)
Bathymetric map: Fig. EUR-25-01.
Names of main islands: The area of island is 0.269 km2.
Number of outflowing rivers and channels (name): 1 (R. Morar).
D2 CLIMATIC
Climatic data at Achnashellach (3)*
Mean temp. [deg C]
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Ann.
3.8
3.2
5.2
6.9
10.1
12.4
13.8
13.6
11.6
8.7
5.7
4.1
8.2
Precipitation [mm]
232
177
127
156
93
114
148
150
189
234
196
242
2,058
* 13-year mean.
Number of hours of bright sunshine: 1,374 hr yr-1.
Fig. EUR-25-01
Bathymetric map [m](2).
Water temperature: Fig. EUR-25-02.
Fig. EUR-25-02
Seasonal change of water temperature [deg C](2).
Freezing period: Occasionally (2).
Mixing type: Monomictic (2).
E. LAKE WATER QUALITY
E1 TRANSPARENCY [m](6)
November 1977 and October 1978: 5.75-10.20.
E2 pH (4)
1977
Depth [m]
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
0-10
-
-
-
-
-
-
-
-
-
-
6.9
6.7
1978
0-10
-
6.6
6.7
-
6.7
-
6.5
6.5
-
6.4
-
-
E6 CHLOROPHYLL CONCENTRATION [micro g l-1]:
Fig.EUR-25-03.
Fig. EUR-25-03
Fluctuation in the concentration of chlorophyll
a. Values refer to the integrated 0-10 m column at open water site (5).E7 NITROGEN CONCENTRATION: Fig. EUR-25-04.
Fig. EUR-25-04
Fluctuation in the concentrations of NO3-N and
NO2-N in the uppermost 10 m of the water column (5).E8 PHOSPHORUS CONCENTRATION (4)
Salmo salar, S. trutta, Salvelinus alpinus, Anguilla anguilla, Gasterosteus
aculeatus.
F4 BIOMASS (7)
Zooplankton: Fig. EUR-25-05.
Fig. EUR-25-05
Seasonal change of zooplankton population [1,000
individuals m-3].
G. SOCIO-ECONOMIC CONDITIONS (1)
G1 LAND USE IN THE CATCHMENT AREA
1978
Area [km2]
[%]
- Natural landscape
Woody vegetation
4.5
3.2
Rough
132.7
93.3
- Agricultural land
0.9
0.6
- Residential area
0.6
0.4
- Others
3.6
2.5
- Total
142.3
100.0
G3 POPULATION IN THE CATCHMENT AREA
1978
Population
Population density [km-2]
Major cities (population)
Total
162
1.0
None
H. LAKE UTILIZATION (3)
H1 LAKE UTILIZATIONSource of water, recreation (sightseeing, swimming, sport-fishing)
and power generation.
I. DETERIORATION OF LAKE ENVIRONMENTS AND HAZARDS (4, 10)
I1 ENHANCED SILTATION
Extent of damage: None.
I2 TOXIC CONTAMINATION
Present status: Not detected.
I3 EUTROPHICATION
Nuisance caused by eutrophication: None.
I4 ACIDIFICATION
Extent of damage: None.
J. WASTEWATER TREATMENTS (1, 10)
J1 GENERATION OF POLLUTANTS IN THE CATCHMENT AREAb) No sources of significant pollution.J3 SANITARY FACILITIES AND SEWERAGE
Municipal wastewater treatment systems: None.
Industrial wastewater treatment systems: None.
N. SOURCES OF DATA
Maitland, P. S. (1981) Introduction and catchment analysis. The Ecology
of Scotland's Largest Lochs, Lomond, Awe, Ness, Morar and Shiel (ed. Maitland,
P. S.), pp. 1-27. Dr. W. Junk Publishers, The Hague.
Smith, I. R., Lyle, A. A. & Rosie, A. J. (1981) Comparative physical
limnology). Ibid., pp. 9-65.
Muller, M. J. (1982) Selected Climatic Data for a Global Set of Standard
Stations for Vegetation Science. 306 pp. Dr. W. Junk Publishers, The Hague.
Bailley-Watts, A. E. & Duncan, P. (1981) Chemical characterisation,
a one-year comparative study. The Ecology of Scotland's Largest Lochs,
Lomond, Awe, Ness, Morar and Shiel (see above), pp. 67-89.
--- (1981) The phytoplankton. Ibid., pp. 91-118.
--- (1981) A review of macrophyte studies. Ibid., pp. 119-134.
Maitland, P. S., Smith, B. D. & Dennis, G. M. (1981) The crustacean
zooplankton. Ibid., pp. 135-154.
Smith, B. D., Maitland, P. S., Young, M. R. & Carr, M. J. (1981) Ibid.,
pp. 155-203.
Maitland, P. S., Smith, B. D. & Adair, S. M. (1981) The fish and fisheries.
Ibid., pp. 223-251.