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searching for Clastic wedge 86 found (97 total)

Fram Formation (458 words) [view diff] exact match in snippet view article find links to article

in the formation. The Fram Formation is a Middle to Upper Devonian clastic wedge forming an extensive continental facies consisting of sediments derived

Mount Townsend (Washington) (322 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Scott (Washington) (486 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Geology of Nunavut (882 words) [view diff] exact match in snippet view article find links to article

Devonian, generating potential red bed related copper deposits in a thick clastic wedge. The Ellesmerian orogeny produced Mississippi-valley type zinc-lead

Bailey Range (785 words) [view diff] exact match in snippet view article find links to article

of the Bailey Range: The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Anderson (Washington) (512 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Tetraxylopteris (1,053 words) [view diff] case mismatch in snippet view article find links to article

discovered in two locations. T. schmidtii was named from the Catskill Clastic Wedge, New York State, United States of America, in rocks of Middle to Upper

Mount Skokomish (441 words) [view diff] exact match in snippet view article find links to article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Boulder Ridge (377 words) [view diff] exact match in snippet view article find links to article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Mathias (459 words) [view diff] exact match in snippet view article find links to article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

The Needles (Olympic Mountains) (635 words) [view diff] exact match in snippet view article

from near Port Townsend The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Walkinshaw (557 words) [view diff] exact match in snippet view article find links to article

climbing Mount Walkinshaw. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Stephen Peak (413 words) [view diff] exact match in snippet view article find links to article

July through September. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Claywood (484 words) [view diff] exact match in snippet view article find links to article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Pershing (423 words) [view diff] exact match in snippet view article find links to article

climbing this mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Steeple Rock (Washington) (498 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are made up of obducted clastic wedge material and oceanic crust. They are primarily Eocene sandstones, turbidites

Mount Deception (Washington) (880 words) [view diff] exact match in snippet view article

June through September. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Sentinel Peak (Jefferson County, Washington) (436 words) [view diff] exact match in snippet view article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

White Mountain (Olympic Mountains) (382 words) [view diff] exact match in snippet view article

weather for climbing. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Elk Mountain (Clallam County, Washington) (510 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Martin Peak (Olympic Mountains) (434 words) [view diff] exact match in snippet view article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Ferry (490 words) [view diff] exact match in snippet view article find links to article

viewing and climbing. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Aries (mountain) (421 words) [view diff] exact match in snippet view article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Ruth Peak (409 words) [view diff] exact match in snippet view article find links to article

July through September. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Noyes (Washington) (571 words) [view diff] exact match in snippet view article

climbing this mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

McCartney Peak (495 words) [view diff] exact match in snippet view article find links to article

climbing this mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Inner Constance (380 words) [view diff] exact match in snippet view article find links to article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Muncaster Mountain (513 words) [view diff] exact match in snippet view article find links to article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Henderson (Washington) (404 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Iron Mountain (Jefferson County, Washington) (471 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Welch Peaks (430 words) [view diff] exact match in snippet view article find links to article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Steel (598 words) [view diff] exact match in snippet view article find links to article

Lake Trail – class 1 The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Gray Wolf Ridge (433 words) [view diff] exact match in snippet view article find links to article

in avalanche danger. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Blairmore Group (992 words) [view diff] exact match in snippet view article find links to article

the Ma Butte Formation. The Blairmore Group is a westward-thickening clastic wedge of clastic sediments derived from the erosion of newly uplifted mountains

West Peak (Jefferson County, Washington) (503 words) [view diff] exact match in snippet view article

weather for climbing. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Rocky Peak (Washington) (413 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Sundial (Olympic Mountains) (444 words) [view diff] exact match in snippet view article

or viewing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Cameron (Washington) (518 words) [view diff] exact match in snippet view article

climbing this mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Fricaba (455 words) [view diff] exact match in snippet view article find links to article

climbing Mount Fricaba. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Meany (603 words) [view diff] exact match in snippet view article find links to article

weather for climbing. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Cruiser (479 words) [view diff] exact match in snippet view article find links to article

weather for climbing. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount LaCrosse (530 words) [view diff] exact match in snippet view article find links to article

climbing the mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Eagle Point (Olympic Mountains) (404 words) [view diff] exact match in snippet view article

slope below Eagle Point. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Fromme (Washington) (532 words) [view diff] exact match in snippet view article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Tom (Washington) (562 words) [view diff] exact match in snippet view article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Unicorn Peak (Olympic Mountains) (549 words) [view diff] exact match in snippet view article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Cat Peak (623 words) [view diff] exact match in snippet view article find links to article

viewing and climbing. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Fairchild (682 words) [view diff] exact match in snippet view article find links to article

July through September. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Appleton (474 words) [view diff] exact match in snippet view article find links to article

in 1.5 mile (2.4 km). The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Warrior Peak (455 words) [view diff] exact match in snippet view article find links to article

climbing the mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Seattle (Washington) (621 words) [view diff] exact match in snippet view article

climbing this mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Athena (Olympic Mountains) (536 words) [view diff] exact match in snippet view article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Angeles (450 words) [view diff] exact match in snippet view article find links to article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Pulitzer (Washington) (556 words) [view diff] exact match in snippet view article

viewing and climbing. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Crystal Peak (Olympic Mountains) (559 words) [view diff] exact match in snippet view article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Constance (928 words) [view diff] exact match in snippet view article find links to article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Pyramid Mountain (Clallam County, Washington) (404 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Adelaide Peak (Washington) (585 words) [view diff] exact match in snippet view article

climbing Adelaide Peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Fitzhenry (458 words) [view diff] exact match in snippet view article find links to article

July through September. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Jefferson Peak (559 words) [view diff] exact match in snippet view article find links to article

climbing this mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

O'Neil Peak (569 words) [view diff] exact match in snippet view article find links to article

park's trail system. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Barnes (Washington) (596 words) [view diff] exact match in snippet view article

viewing and climbing. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Ludden Peak (614 words) [view diff] exact match in snippet view article find links to article

viewing and climbing. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Woden (The Valhallas) (621 words) [view diff] exact match in snippet view article

climbing these peaks. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Lena (Washington) (494 words) [view diff] exact match in snippet view article

weather for visiting. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Maiasaura (2,602 words) [view diff] exact match in snippet view article find links to article

Bones and rocks of the Upper Cretaceous Two Medicine-Judith River clastic wedge complex, Montana. In Field trip guidebook, Society of Vertebrate Paleontology

Mount Elk Lick (566 words) [view diff] exact match in snippet view article find links to article

Favero, and Frank King. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Delabarre (579 words) [view diff] exact match in snippet view article find links to article

climbing this mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Copper Mountain (Mason County, Washington) (543 words) [view diff] exact match in snippet view article

ore on the mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Worthington (Washington) (480 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Wilder (624 words) [view diff] exact match in snippet view article find links to article

climbing this mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Childs (532 words) [view diff] exact match in snippet view article find links to article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Lincoln (Washington) (792 words) [view diff] exact match in snippet view article

Harniss Chute – class 3 The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Zindorf (491 words) [view diff] exact match in snippet view article find links to article

weather for climbing. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Chimney Peak (Olympic Mountains) (644 words) [view diff] exact match in snippet view article

climbing this peak. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Lost Peak (Jefferson County, Washington) (493 words) [view diff] exact match in snippet view article

climbing this mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Maiden Peak (Washington) (525 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Bolivar Coastal Fields (2,932 words) [view diff] exact match in snippet view article find links to article

northeast thickening of the Eocene clastic wedge, the southwest thickening of the Miocene–Holocene clastic wedge, and the main structural and stratigraphic

Mount Mystery (606 words) [view diff] exact match in snippet view article find links to article

climbing this mountain. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Lawson (Washington) (529 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Mount Bretherton (648 words) [view diff] exact match in snippet view article find links to article

weather for visiting. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Geology of the Appalachians (2,593 words) [view diff] exact match in snippet view article find links to article

southeastward-thickening foreland basin. Coal and associated rocks form a clastic wedge that thickens from north to south, from Pennsylvania into southeast

Blue Mountain (Washington) (636 words) [view diff] exact match in snippet view article

cover during the summer. The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and

Two Medicine Formation (3,049 words) [view diff] exact match in snippet view article find links to article

Bones and rocks of the Upper Cretaceous Two Medicine-Judith River clastic wedge complex, Montana. In Field trip guidebook, Society of Vertebrate Paleontology

Olympic Mountains (7,559 words) [view diff] exact match in snippet view article find links to article

northeastern portion of the mountains. The Olympics are made up of obducted clastic wedge material and oceanic crust. They are primarily Eocene sandstones, turbidites

Delta Field (Niger Delta) (2,353 words) [view diff] exact match in snippet view article

in the delta. The stratigraphy of the Niger Delta is complicated by clastic wedge syndepositional collapse that occurred as the result of marine shales