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Red Wing Minnesota

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Series: GSA Field Guide
Published: 01 January 2011
DOI: 10.1130/2011.0024(18)
EISBN: 9780813756240
... of Goodhue County. Geophysical Survey ABSTRACT Red Wing, Minnesota, is located in the upper Mississippi River valley near the northern margin of the Driftless Area, a portion of southeast Minnesota and western Wisconsin that was not glaciated in the late Quaternary characterized by river valleys...
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Figure  5 —Representative cranidia and pygidia of  Praepatokephalus  specie...
Published: 01 September 2005
, locality 4, ×3.7; 2, medium cranidium (CMNH 52660), from Oneota Dolomite near Red Wing, Minnesota, ×5.8; 3, large pygidium (CMNH 52661) from same locality as 2, ×7.5; 4–6, Praepatokephalus sp. B, all testate and from 3.28 m above the base of the Stonehenge Limestone near Bellefonte, Pennsylvania
Journal Article
Journal: GSA Bulletin
Published: 01 January 1941
GSA Bulletin (1941) 52 (1): 49–60.
... of the Jordan-Oneota contact rises from 200 feet above sea level in the region of Austin to over 1150 feet on the crest of a local high to the southwest of Winona. Faults occur along the valley of the St. Croix River north of Stillwater and along the Mississippi valley at Hastings and Red Wing. University...
Journal Article
Published: 01 September 2005
Journal of Paleontology (2005) 79 (5): 1021–1027.
..., locality 4, ×3.7; 2, medium cranidium (CMNH 52660), from Oneota Dolomite near Red Wing, Minnesota, ×5.8; 3, large pygidium (CMNH 52661) from same locality as 2, ×7.5; 4–6, Praepatokephalus sp. B, all testate and from 3.28 m above the base of the Stonehenge Limestone near Bellefonte, Pennsylvania...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2007
GSA Bulletin (2007) 119 (3-4): 363–376.
... respond to past climate change. A three-dimensional surface-water–groundwater model was developed to assess the effects of mid-Holocene climate change on water resources within the Crow Wing Watershed, Upper Mississippi Basin in north central Minnesota. The model was first calibrated to a 50 yr historical...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1959
AAPG Bulletin (1959) 43 (3): 654–662.
... County, Minnesota, have been dated by the K-A technique. The samples were collected and prepared by W. E. Crain (1957). KA 113 is from a sandy, highly glauconitic layer 6½ feet above the base of a roadcut on Country Road 34, approximately 3 miles west of Red Wing ( Fig. 1 ), SW.¼, Sec. 27, T. 113N., R 15...
FIGURES
Journal Article
Journal: Geology
Published: 14 October 2022
Geology (2022) 50 (12): 1398–1402.
...Vera A. Korasidis; Scott L. Wing; David M. Nelson; Allison A. Baczynski Abstract Plant megafossils from the Paleocene-Eocene Thermal Maximum (PETM) in the Bighorn Basin, north-central Wyoming, USA, document a dramatic shift in floral composition, whereas palynofloral change from the same sections...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1958
AAPG Bulletin (1958) 42 (1): 173–189.
..., partly metamorphosed sequence of argillites, cherty iron formations (taconites), and quartzites perhaps 5,000–10,000 feet thick, in narrow northeast-trending belts in Morrison, Crow Wing, and Aitkin counties, Minnesota. Alteration of the original cherty and shaly rocks to granular pseudoquartzites...
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Series: GSA Field Guide
Published: 01 January 2011
DOI: 10.1130/2011.0024(26)
EISBN: 9780813756240
.... BR—Broule River; BSM—Big Stone Moraine; CH R—Chippewa River; CR—Cannon River; KR—Kettle River; LP—Lake Pepin; MA—City of Mankato; MN R—Minnesota River; MISS R—Mississippi River; NU—City of New Ulm; RW—City of Red Wing; SCM—St. Croix Moraine; SP—City of St. Paul; SR—St. Croix River; TF—Taylors Falls...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1982
AAPG Bulletin (1982) 66 (8): 989–1020.
... water Dolomitization Subtidal, “at surface” Subsurface, interstitial * Modified from Carroll (1979) . Two other structural elements may be significant to basin interpretation: the Red Wing Creek structure and the Newporte structure ( Fig. 2 ). Both of these structures...
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Journal Article
Published: 01 May 2004
Journal of Paleontology (2004) 78 (3): 612–616.
...RICHARD C. FOX Family Palaeoryctidae Winge, 1917 Lainoryctes new genus Abbreviations used in this paper are: SMM, Science Museum, St. Paul, Minnesota; UALVP, Laboratory for Vertebrate Paleontology, University of Alberta, Edmonton; L, length; W, width. Measurements are in millimeters...
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Journal Article
Journal: PALAIOS
Published: 26 March 2020
PALAIOS (2020) 35 (3): 135–150.
... 2004 ; Wings 2004 ; Daniel and Chin 2010 ; Bodzioch 2015 ; Kowal-Linka 2015 ; Previtera 2017 , 2019 ). These diagenetic studies have served to help clarify appropriate protocols and best practices for analyzing vertebrate hard tissues when the goal is to recover paleobiological and paleoclimatic...
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Journal Article
Journal: PALAIOS
Published: 01 October 2011
PALAIOS (2011) 26 (10): 658–664.
... the effects of heat on extant avian eggshell, which is constructed primarily of CaCO 3 deposited within a protein matrix. Ostrich (Struthio camelus) and glaucous-winged gull (Larus glaucescens) eggshell fragments were heated to temperatures up to 800 °C for varying lengths of time. A series of dramatic color...
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Journal Article
Journal: Geosphere
Published: 16 January 2020
Geosphere (2020) 16 (2): 594–618.
... between Hanna Basin and surrounding basins. Red outline indicates study area and outline of Figure 1B . (B) Map of Paleocene–Eocene Hanna Formation outcrops (brown) and structural features (modified after Blackstone, 1993 ). Study area of Figure 3 indicated with white box; geologic unit contacts...
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Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2007.2427(16)
... the wing membrane, which may not have offered much nutrient to the predators; and (2) the strong wing membrane, which would have secured the wing elements while the muscle mass would have fallen away. In either case, the wing membrane may have served as a protective layer over the forelimb bones until...
Journal Article
Journal: Economic Geology
Published: 01 August 2018
Economic Geology (2018) 113 (5): 1161–1179.
...V. Taranovic; E. M. Ripley; C. Li; S. B. Shirey Abstract The Tamarack Intrusive Complex (1105 ± 1.2 Ma), in northeastern Minnesota, occurs within the Midcontinent rift system and hosts potentially economic Ni-Cu-(PGE) mineralization. The system represents “conduit-style” mineralization and with 1.3...
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Journal Article
Journal: Economic Geology
Published: 01 January 2013
Economic Geology (2013) 108 (1): 45–58.
... in the Archean atmosphere (e.g., Farquhar and Wing, 2003 ). Anomalous Δ 33 S values have been utilized by Bekker et al. (2009) to confirm the importance of crustal S in komatiite-related deposits. For magmatic deposits where Archean rocks are unlikely to have supplied S to the magma, Δ 33 S will be of little...
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Journal Article
Published: 01 January 2011
Journal of Paleontology (2011) 85 (1): 1–21.
..., 1967 ; Tschudy, 1966 , 1975 , 1976 ) with only four comprehensive floras published from localities east of the Western Interior Basin (all of Cenomanian age: Iowa, Schemel, 1950 and Hall, 1963 ; Minnesota, Hall and Peake, 1968 ; Kansas, Kovach and Dilcher, 1988 ). Occasionally megaspores...
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Journal Article
Published: 01 January 2013
Journal of Paleontology (2013) 87 (1): 16–43.
.... and M. Stark of Riceville, Iowa, T. Stenerson of Red Wing, Minnesota, H. L. Strimple (deceased), and B. Witzke of the Iowa Geological Survey. None of the papers in this series would have been possible without their efforts. Field work was aided by M. Ayers of Humboldt, Iowa, the Cantine family...
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Journal Article
Published: 01 September 2011
Journal of Sedimentary Research (2011) 81 (9): 656–669.
... to the void network. E , F) Matrix of micrite, peloids (p), and silt-size skeletal debris (white arrows) that may be bright orange, dull red, or nonluminescent. Cements (c) are dominantly nonluminescent zone 1 calcites, although minor amounts of luminescent zones 2 cement can be present. This figure...
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