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@@ -30,8 +30,8 @@ accumulation value that will initiate a new stream. If Montgomery's
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method for channel initiation is used, the cell value of the
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method for channel initiation is used, the cell value of the
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accumulation input map is multiplied by <tt>(tan(local
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accumulation input map is multiplied by <tt>(tan(local
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slope))<sup>mexp</sup></tt> and then compared
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slope))<sup>mexp</sup></tt> and then compared
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-to <b>threshold</b>. If <b>mexp</b> is given than the method of
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-Montgomery and Foufoula-Georgiou (1993) to initiate a stream with this
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+to <b>threshold</b>. If <b>mexp</b> is given, then the method of
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+Montgomery and Foufoula-Georgiou (1993) is used to initiate a stream with this
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value. The cell value of the accumulation input map is multiplied
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value. The cell value of the accumulation input map is multiplied
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by <tt>(tan(local slope))<sup>mexp</sup></tt> and then compared
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by <tt>(tan(local slope))<sup>mexp</sup></tt> and then compared
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to <b>threshold</b>. If threshold is reached or exceeded, a new stream
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to <b>threshold</b>. If threshold is reached or exceeded, a new stream
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@@ -75,9 +75,9 @@ started and traced downstream to its outlet point. As for
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calculated as the number of cells draining through a cell.
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calculated as the number of cells draining through a cell.
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<p>
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<p>
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-If <b>accumulation</b> is given than the accumulation values of the
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+If <b>accumulation</b> is given, then the accumulation values of the
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provided <b>accumulation</b> map are used and not calculated from the
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provided <b>accumulation</b> map are used and not calculated from the
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-input <b>elevation</b> map. In this case the <b>elevation</b> map must
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+input <b>elevation</b> map. In this case, the <b>elevation</b> map must
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be exactly the same map used to calculate
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be exactly the same map used to calculate
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<b>accumulation</b>. If <b>accumulation</b> was calculated with
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<b>accumulation</b>. If <b>accumulation</b> was calculated with
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<em><a href="r.terraflow.html">r.terraflow</a></em>, the filled
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<em><a href="r.terraflow.html">r.terraflow</a></em>, the filled
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