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Picture of unglaciated unconfined reach

Cache la Poudre River at Indian Meadows

(Photo by Lina Polvi)

Picture of vegetation around unglaciated unconfined reach

Narrow-leaf cottonwoods and blue spruce are most common along stream bank (lower-left)


Unconfined left bank of N. St. Vrain

(Photo by Lina Polvi)

Types of Riparian Vegetation

(Information compiled by Lina Polvi)

Because unglaciated process domains are located in the Lower Montane ecotone, vegetation types in unglaciated unconfined areas will be the riparian species found in the Montane region. These include narrowleaf cottonwood and blue spruce as well as western birch and alder.

Wetlands are likely to form in unconfined valleys due to increased groundwater, floodplain microtopography creating depresssions, and possibly beaver dams. Although wetlands are not necessarily considered riparian zones, when they form in proximity to a stream they will influence the type and extent of riparian vegetation. More cottonwoods will be present than other vegetation types found in other unglaciated process domains. Cottonwood communities are early, mid- or late seral. Healthy riparian areas support all stages of cottonwood communities.

Lower montane vegetation table

Controls on Riparian Vegetation Growth

In these broad valleys, the hill slopes do not have a great influence on floodplain processes, including riparian vegetation growth.

Other ecosystem processes probably play a greater role:

Vegetation community type

Groundwater influence


Click a link below to learn more about riparian vegetation in each process domain:

Colluvial Hollows Ephemeral Channels Glaciated Confined Glaciated Partially Confined Glaciated Unconfined Unglaciated Confined Unglaciated Partially Confined Unglaciated Unconfined
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