![]() How do waterfalls form? The Cascade Range is made of volcanic layers from numerous eruptions over the last 35+ million years. The layers, or deposits, originated from numerous sources, each having a different resistance to erosion. They were then uplifted after the volcanic activity stopped. The stream’s erosive energy continues to carve the channels that we see today. |
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![]() Follows along a series of rock steps |
![]() Descends as the stream diverges into 2 or 3 parts |
![]() Descends from a wide stream |
![]() Descends from a distinct series of seperate falls |
![]() Descends from a constricted width of a stream into a pool below |
![]() Descends vertically, losing contact with the bedrock below |
![]() Descends vertically maintaining some contact with the bedrock surface |
![]() Similar to horsetail form, with an increasing width of spray |
**Information adapted with permission from the Waterfall Lover's Guide to the Pacific Northwest, by G.A. Plumb, The Mountaineers, Seattle, WA.