Module 3
Catchment - Scale Controls on River Geomorphology
Logan River Watershed (a 10 digit HUC)
Logan River Watershed (a 10 digit HUC)
Distance: 45,700m, Elevation: 1605m—At this knick point, the elevation profile seems off due to the river underneath the hill and the hill elevation being recorded instead of the rivers.
Distance: 36500m, Elevation:1528m — the third dam is located at this knick point.
Distance: 35200m, Elevation: 1512 m—At this knick point, it seems there is a campground on the river left and a parking lot a couple of meters ahead on the river right, which the infrastructure could have caused.
Distance: 34000m, Elevation:1512m — The Second dam is located here at this knick point.
Distance: 30,800m, Elevation:1431m — The First Dam is located at this knick point.
4206ft Great Salt Lake
Used google earth pro and selected at the entrance of the Bear River to the Great Salt Lake.
5000 ft Lake Bonneville
82 km
172,404.1 m = 172.4041 km
Calculated using the calculate geometry tool on the Logan Rivers Watersheds field titled shape_length, set the property to perimeter length and length unit to meters.
For the perennial drainage network of the Logan River:
The stream order of the Logan River at its mouth. 5
The stream order of Temple Fork at its mouth. 3
The stream order of Beaver Creek. 1
⬇️Below are maps of the drainage network, in blue is the perennial drainage network with stream names.
It does as there are relatively more first-order streams than second-order and third-order streams, so the number of streams decreases as a stream order increases. Also, the average length of streams increases when stream order does. Lastly, the high-order stream drainage areas are larger than the small-order stream drainage areas. Logan River being in line with Hortonian laws of streams network means that the drainage network for the Logan River has a more natural and organized drainage network.