Total elevation change: Max (8,095 ft) - min (4,408 ft) = 3,687 ft (1.1 km)
Base-level control of the Logan River today
Base level is the level to which a channel naturally cuts. Dams and geology control base-level today. The main base level feature currently is Cutler Reservoir at 4,414 ft.
Base level control of the Logan River 18,000 yrs ago
18,000 yrs ago Lake Bonneville was around the level of the Shoreline (~4,850ft), so this lake elevation would be a strong base level control at that point in time.
Mainstem Length: 54 miles (86 km)
Concavity
Concavity = 2A/H
= 2(350 m) / 1,100 m
= 0.6
Knickpoints and hypotheses about controls
There is a knickpoint between miles 45 and 47 that coincides with an unnamed spring entering the River in the upper watershed. Perhaps there is stronger bedrock here so less downcutting.
There is a knickpoint between miles 22 and 20, coinciding with third dam, and second dam, affecting normal river downcutting. Dams first slow, but then accelerate downcutting downstream.
There is also possibly another knickpoint at the mouth of the canyon, coinciding with first dam, although this is hard to tell because of the transition from confined to unconfined valley.
Catchment length
48 km along the longest axis
Catchment area
646 km2
Catchment perimeter length
172 km
Circularity ratio
Rc= A/ Ac
646km2 / 729 * 3.14 = 0.28
Elongation ratio
Er= A^0.5 / L
25.4 /48 = 0.53
Form factor
Rf = A/L^2
646/2304 = 0.28
Catchment relief
Emax- Emin
9979 -4,414 ft = 5565 ft = 1696 m
Relief ratio
Rh= H/L
1696 / 48 m = 35
Drainage density
Dd = total length of stream channels/ area of catchment
197 /646km2 = 0.3 km /km2
Drainage pattern
Dendritic and maybe a little trellis in spots.
Stream order of Logan River at mouth
6
Stream order of Temple Fork at its mouth
4
Stream order of Beaver Creek
4
Does the Logan River obey Hortonian laws of stream network composition?
As stream order increases...
the quantity of streams of a given stream order decrease. YES ...many first order streams, and less streams with 4 ,5, and 6 order.
mean stream length increases. YES, seems that ones are shorter than those with a larger stream order.
catchment area increases. YES, this once seems the most intuitive. Higher order streams are draining greater areas.