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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Banks Island (2)
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Canada
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Arctic Archipelago (2)
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Mackenzie Mountains (2)
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Western Canada
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Alberta (4)
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British Columbia (1)
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Northwest Territories (4)
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Saskatchewan (4)
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North America
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Great Plains
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Northern Great Plains (2)
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Western Interior (1)
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United States
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Montana
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Glacier County Montana (1)
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elements, isotopes
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halogens
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chlorine
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Cl-36 (1)
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isotopes
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radioactive isotopes
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Cl-36 (1)
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fossils
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Chordata
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Vertebrata
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Tetrapoda
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Mammalia (2)
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Invertebrata (1)
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geochronology methods
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Blancan (1)
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Quaternary
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Irvingtonian (2)
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Matuyama Chron (7)
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upper Pleistocene
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Wisconsinan
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upper Wisconsinan (1)
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upper Quaternary
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Brunhes Chron (7)
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Tertiary
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Neogene
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Miocene
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upper Miocene (1)
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Pliocene
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Gauss Chron (2)
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upper Pliocene (4)
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upper Tertiary (2)
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upper Cenozoic (7)
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Laurentide ice sheet (1)
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igneous rocks
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igneous rocks
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volcanic rocks
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basalts (1)
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Primary terms
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Canada
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Arctic Archipelago (2)
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Mackenzie Mountains (2)
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Western Canada
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Alberta (4)
-
British Columbia (1)
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Northwest Territories (4)
-
Saskatchewan (4)
-
-
-
Cenozoic
-
Blancan (1)
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Quaternary
-
Cordilleran ice sheet (1)
-
lower Quaternary (1)
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Pleistocene
-
Irvingtonian (2)
-
lower Pleistocene (3)
-
Matuyama Chron (7)
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upper Pleistocene
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Wisconsinan
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upper Wisconsinan (1)
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-
-
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upper Quaternary
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Brunhes Chron (7)
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-
-
Tertiary
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Neogene
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Miocene
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upper Miocene (1)
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Pliocene
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Gauss Chron (2)
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upper Pliocene (4)
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upper Tertiary (2)
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upper Cenozoic (7)
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Chordata
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Vertebrata
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Tetrapoda
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Mammalia (2)
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climate change (1)
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geochronology (8)
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geomorphology (1)
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glacial geology (1)
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igneous rocks
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volcanic rocks
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basalts (1)
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Invertebrata (1)
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isotopes
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radioactive isotopes
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Cl-36 (1)
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North America
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Great Plains
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Northern Great Plains (2)
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Western Interior (1)
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paleoclimatology (2)
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paleoecology (1)
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paleomagnetism (13)
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sedimentary rocks
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clastic rocks
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diamictite (1)
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sedimentation (4)
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sediments
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clastic sediments
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loess (2)
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till (5)
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stratigraphy (4)
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United States
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Montana
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Glacier County Montana (1)
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weathering (1)
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sedimentary rocks
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sedimentary rocks
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clastic rocks
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diamictite (1)
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volcaniclastics (1)
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sediments
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sediments
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clastic sediments
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boulders (1)
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colluvium (2)
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drift (1)
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erratics (1)
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gravel (1)
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loess (2)
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silt (2)
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till (5)
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-
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volcaniclastics (1)
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soils
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paleosols (4)
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Lithostratigraphy and paleomagnetism of pre-Fraser glacial deposits in south-central British Columbia
Stratigraphy and paleomagnetism of Late Pliocene and Pleistocene sediments in the Wellsch Valley and Swift Current Creek areas, southwestern Saskatchewan, Canada
Magnetostratigraphy of Quaternary and late Tertiary sediments on Banks Island, Canadian Arctic Archipelago
Stratigraphy and paleomagnetism of the Late Miocene Davis Creek silt, East Block of the Cypress Hills, Saskatchewan
Late Tertiary to late Quaternary record in the Mackenzie Mountains, Northwest Territories, Canada: stratigraphy, paleosols, paleomagnetism, and chlorine - 36
Paleomagnetic evidence for late Cenozoic glaciations in the Mackenzie Mountains of the Northwest Territories, Canada
A record of Early Pleistocene glaciation on the Mount Edziza Plateau, northwestern British Columbia
Paleomagnetism of tills and associated paleosols in southwestern Alberta and northern Montana: evidence for Late Pliocene–Early Pleistocene glaciations
Paleomagnetism of Quaternary and late Tertiary sediments on Mokowan Butte, southwestern Alberta
Stratigraphy and paleomagnetism of the Jaw Face section, Wellsch Valley site, Saskatchewan
Late Cenozoic paleomagnetic record of Duck Hawk Bluffs, Banks Island, Canadian Arctic Archipelago
Davis Creek silt, an Early Pleistocene or Late Pliocene deposit in the Cypress Hills of Saskatchewan
Stratigraphy, paleomagnetism, and vertebrate paleontology of Quaternary preglacial sediments at the Maser-Frisch Site, southeastern Alberta
Abstract The Milk River Canyon is located in southeastern Alberta some 62 mi (100 km) east of the town of Coutts (Fig. 1). Access to a valley overlook by passenger caron paved and unpaved county roads is relatively easy and requires no permissions to cross private land, but the easternmost unpaved section of road (beyond Black Butte, Fig. 2 is to be avoided if wet. The canyon itself is not visible until the overlook on its rim is reached. The map (Fig. 2 shows readily recognizable points on the route from Coutts and indicates distances between conspicuous landmarks. As is customary, barbed wire gates, if encountered, should be left as found: open if open, closed if closed. There are no services available east of Coutts, so gas tanks should be comfortably filled.