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Cloudcap - Prominent Geological Features of Crater Lake National Park
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The topmost lavas on the caldera wall overlooking Cloudcap Bay are glassy dacites not unlike those of the Llao, Grouse Hill, and Cleetwood flows. They were likewise erupted after the andesitic phase of Mazama's activity had come to
an end. Two main flows may be distinguished: an older one to the south, which seems to have had its source beneath Cloudcap, and a much thicker
flow farther north, the Redcloud flow, which escaped from a vent on the caldera wall. The relations between them are indicated on the panorama .... [The
Northern Arc of Vents: Dacites of Redcloud and Cloudcap, The Geology of Crater Lake National Park, Oregon (1942) by Howell Williams] |

View east with Mount Scott in background, Redcloud Cliff at upper left (v-shaped flow formation), and Cloudcap (green tree cover) at upper center above pumice castle (orange
rock formation in caldera wall), photo by Robert Mutch |
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Note: the numbers associated with each feature
name above correspond to their place on the Custom Google Map below
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Crater Lake National Park
Prominent Geological Features Map
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