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U-shaped glacial valley and paternoster lakes

Carthew Lakes form a series of paternoster lakes in the upper reaches of a glacial valley in Waterton Lakes National Park, Alberta, Canada. (090710-25)
Download ImageLimestone cliffs, southern Alberta.

Paleozoic LImestone cliffs, southern Alberta, Canada. (090709-24)
Download ImageTalus Cones (vertical)

Talus cones, built through the accumulation of rock debris, fallen from the cliffs above. Banff National Park, Canada. (ID: 090707-14)
Download ImageBraided River and Canadian Rockies

The Kicking Horse River forms a braided river pattern as it flows through the Canadian Rockies in Yoho National Park, Canada. (090707-2)
Download ImageDrumlin, southern Alberta (Pan).

Drumlin, a depositional feature of continental ice sheets, southern Alberta, Canada. Ice flowed from left to right. (090709-19pan)
Download ImageDrumlin, southern Alberta.

Drumlin, a depositional feature of continental ice sheets, southern Alberta, Canada. Ice flowed from left to right. (090709-13)
Download ImageCleavage and bedding in limestone and shale.

Cleavage and bedding in gently folded limestone and shale, Yoho National Park, British Columbia, Canada. (090706-19)
Download ImageTalus Cones

Talus cones, built through the accumulation of rock debris, fallen from the cliffs above. Banff National Park, Canada. (ID: 090707-17)
Download ImageEocene Pillow Basalt, Washington (vertical)

Cliff exposure of Eocene pillow basalt of the accreted Siletzia Terrane (Crescent Formation). the pillow shapes result from the basalt being erupted underwater. Olympic National Park, WA. (090630-87)
Download ImageErosion of a natural bridge

Erosion of a natural bridge in limestone, Yoho National Park, British Columbia, Canada. (090706-49)
Download ImageAlkali lake, British Columbia, Canada.

Evaporating alkali lake in the Okanogan of. Note how it leaves behind zones of precipitated minerals. (090704-54)
Download ImageIntrusive contact (vertical)

Contact of granitic igneous rock (tonalite) with metamorphic rock (slate). Note the small sills (apophyses) which invade the country rock. (090704-14)
Download ImageFolded pegmatite dike in slate.

Folded pegmatite in slate, likely caused by dissolution of the slate. Note the cleavage planes in the slate are parallel to the axial surface of the fold, southern British Columbia, Canada. (090704-2).
Download ImageTalus cone and cliffs, southern BC, Canada.

Rock fall and debris flows from the cliffs creates a cone of talus. (090704-34)
Download ImageTilted marine sandstone, Washington

Tilted marine sandstone of the uplifted Olympic subduction complex, Mt. Angeles, Olympic National Park, Washington. (090630-63)
Download ImageRaplee Monocline, SE Utah

San Juan River flows through folded rocks of the Raplee Anticline, SE Utah. (090321-73)
Download ImageAngular unconformity, central Utah.

Angular unconformity and channel deposit, central Utah. Henry Mtns in background. (090322-37)
Download ImageGraphic Granite

detail view of graphic granite –intergrown quartz and k-feldspar. Approx 4 cm across. (090506-13)
Download ImageAngular unconformity, Utah (Pan).

Angular unconformity and channel deposit, central Utah.(090322-32)
Download Image
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