GUELPH, ONTARIO - Agriculture and Agri-Food Canada
GUELPH, ONTARIO - Agriculture and Agri-Food Canada
GUELPH, ONTARIO - Agriculture and Agri-Food Canada
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The action of ice <strong>and</strong> water was such that the deposits were badly deformed.<br />
As a result the topography of soils developed on these materials consists of’<br />
irregular steep slopes.<br />
Glacio-fluvial materials occur most commonly in the western portion of<br />
the County.<br />
6. Outwash<br />
Outwash materials are scattered throughout the County <strong>and</strong> are<br />
commonly found in the vicinity of th e stream courses.<br />
most<br />
Outwash is t)he term used for stratified drift that is stream built. Such<br />
material is well sorted <strong>and</strong> the average grain size diminishes downstream while<br />
the degree of roundness rapidly increases. The material is usually s<strong>and</strong> <strong>and</strong><br />
gravel deposited in smooth gently sloping outwash plains <strong>and</strong> terraces.<br />
The deptJh of the outwash material is quite variable. It may vary in depth<br />
from one to twenty feet; in some cases it is underlain by compact till while in<br />
other places, particularly in the northern part of the County, it is underlain<br />
by bedrock.<br />
7. Limestone Bedrock<br />
The limestone bedrock outcrop occurs most commonly on the Bruce Peninsula.<br />
In some localities a shallow covering of till, outwash or organic material<br />
may occur over the bedrock. In such areas shallow soils may have formed.<br />
Therefore, the area delineated as the limestone bedrock varies widely in texture,<br />
t)opography <strong>and</strong> drainage.<br />
The composition of the limestone<br />
several bedrock formations.<br />
8. Organic<br />
also varies since the area is made up of<br />
The humified remains of trees, herbs <strong>and</strong> mosses make up organic surface<br />
deposits. Organic deposits are common in Bruce County, one of t’he best<br />
examples being the Greenock swamp situated in Greenock Township. The<br />
organic deposit’s occurring in Bruce County are usually well decomposed <strong>and</strong><br />
are designated as muck. They are underlain by s<strong>and</strong>, clay or marl. Their<br />
reaction is approximately neutral <strong>and</strong> the topography is level to depressional.<br />
Relief<br />
The elevation of t’he l<strong>and</strong> in Bruce County is indicated by the brown contour<br />
lines on the enclosed soil map. The altitude ranges from 600 to 1,025 feet<br />
above sea level. The highest part of the County is in the Walkerton district<br />
from where the elevation falls toward Lake Huron.<br />
One of the important factors related to soil formation <strong>and</strong> soil management<br />
is the topography or relief of the l<strong>and</strong>. The degree of slope influences drainage;<br />
run-off of surface water, <strong>and</strong> erosion, <strong>and</strong> in some instances restricts the use<br />
of farm machinery. The average slope of the topographic classes <strong>and</strong> the total<br />
area of each slope group are given in Table 4. The major distribution of the<br />
topographic classes in Bruce County are shown in Figure 6.<br />
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