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Lake Information

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 Vital Lake Statistics
Source: Crowe Valley Conservation Authority (CVCA) -
1994
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Size
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2,000 acres / 809 hectares
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Shoreline
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Approximately 47 miles / 80km
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Depth
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Average depth is 15 feet / 5 metres, with deep
holes
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Deepest point
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24 metres
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Summer level
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262.16 metres above sea level
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Winter level
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261.7 metres above sea level
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100 year Flood
(the level the lake is likely to reach once every 100 years, or
the Authoritys worst case scenario)
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262.70 metres above sea level
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Lake Kasshabog's Dam
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Reconstructed in 1956
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Owned by Ontario Ministry of Natural Resources (MNR)
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Lake level controlled by Crowe Valley Conservation Authority
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6.71 m long by 3.55 m high
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Single bay of logs 4.27 m long
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7 logs at 0.25 m x 0.30 m
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1 log at 0.25 m x 0.15 m
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Fall drawdown commences annually at October 15
 Lake Levels and Surveys
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The regulated lake level was established in the early 1950s
by the Department of Lands and Forests.
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Reviewed and maintained in 1960s by the Department of Lands
and Forests.
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Altered in 1978 and again in 1981 by CVCA in cooperation with MNR.
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Lake bottom mapped in 1961 by CVCA. Lake surveyed by MNR in 1973,
and updated in 1979.
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The CVCA monitors the lake level of Lake Kasshabog via electronic
gauge located on the south side of Connor Bay (its the concrete
and steel structure on the waters edge near the landing off
South Connor Bay Road). Levels are recorded every 4 hours. There are
2 staff gauges; one located at the west end of the dam, and the other
at Stoney Point Marina.
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The land surrounding the lake is typical of the Precambrian Shield,
with bare rock ridges, and shallow till. Much of the surrounding area
is pocked by low wet areas, with organic bottom deposits.
 Location, Development,
Water Quality
Source: Ontario Ministry of the Environment - 1978
Kasshabog Lake is located approximately 22 km north of Havelock in Methuen
Township. The lake receives flow from several smaller tributary lakes.
The major inflow is from the North River which is part of the Crowe Lake
system (see separate flow sheet). Although the lake has many islands and
bays, only MacDonald (Bills) Bay appeared to be hydrologically separated
from the main lake. In 1978, the lake had 16 permanent residences, 504
cottages, and 4 cottage rental units. In addition, MacDonald Bay had 81
cottages along its shoreline. The volume of water in MacDonald Bay flushed
itself about twice during the year, while the rest of the lake flushed
only about once a year.
Kasshabog Lake had soft, slightly acidic water with a moderately low
amount of apparent colour. The hardness, alkalinity, and conductivity
levels indicated the lake was well mixed. Thermal stratification (temperature
layers) were noted in almost all the bays and monitoring stations. Water
clarity was moderately good throughout the lake, and the secchi disk results
indicate the lake is mesotrophic, or moderately enriched.
Dissolved oxygen distribution throughout the lake showed a gradual decline
with increasing depth, probably due to the decomposition of organic matter
in the bottom waters. No significant accumulations of nutrients in the
bottom waters was noted at any of the monitoring stations.
The density and composition of the phytoplankton (microscopic water plants)
indicated an unenriched lake condition. The density and composition
of the zookplankton (microscopic animals) indicated moderately enriched
lake conditions.
***
In summary, Lake Kasshabog had good water quality during
1978, but is considered oilgotrophic, bordering on mesotrophic. Any further
shoreline development on the lake should be carefully planned and constructed
to minimize or eliminate the addition of plant nutrients to the lake.
 Soils and Climate
Source: OMAFRA Soils of Peterborough County,
Report No. 45 Ontario Institute of Pedology 1981
(Pg. 9)
Much of the Northern part of the County is under forest and managed
by the Ontario Ministry of Natural Resources
There are extensive
areas suitable for recreational use around the numerous lakes. Thousands
of cottages dot the shorelines; many developments are under way to meet
the almost insatiable demand for recreational land.
Strict controls on cottage density and sewage and garbage disposal must
be maintained if eutrophication of lakes and unsightly environment are
to be avoided. Many shorelines are rocky with thin soil cover and unsuitable
for septic tanks unless costly installation procedures are followed.
(pg. 8)
There is a large hectarage of very poorly drained depression basins in
the southern part of the county with water table levels at or near the
surface for most of the year. These are valuable holding basins retaining
large quantities of water which would be drained away and lost to the
county. Most of these areas should remain in their undrained state to
aid in maintaining groundwater levels.
 Climactic Data
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Elevation
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262 metres above sea level
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Mean annual temperature
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6 C
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Mean April temperature
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11 C
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Mean July temperature
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26 C
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Mean October temperature
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14 C
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Mean annual precipitation
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80 cm
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Sportfish of Kasshabog
The joy of catching a fish is a great one; let's keep the opportunity
alive by practicing "Catch and Release", so the fish can spawn
another generation of rod-bending offspring!!!
Remember to take care when fishing on the bottom near-shore - there
are underwater phone lines, water intakes, and anchor lines all ready
to grab your favourite lure!
The information below is a compilation, including information from
The Ontario Ministry of Natural Resources, Ontario Federation of Anglers
and Hunters, and the Lake Kasshabog Residents' Association, Inc.
Sportfish in Lake Kasshabog include: smallmouth bass, muskellunge,
rock bass, and largemouth bass.

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