Geology of the Ponca Creek and Keya Paha River Drainage Basins in Nebraska

The geology of the study area has been investigated many times over more than a century. Interested readers are directed to the report by Diffendal and Voorhies (1994), which gives a more detailed overview of the results of the investigations and lists most of the more important reports about the ar...

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Main Author: Diffendal, Robert F., Jr.
Format: Text
Language:unknown
Published: DigitalCommons@University of Nebraska - Lincoln 1997
Subjects:
Online Access:https://digitalcommons.unl.edu/diffendal/51
https://digitalcommons.unl.edu/context/diffendal/article/1051/viewcontent/Archaeological_Survey_Ponca_Keya_Paha_Diffendal_Sep_97_REV.pdf
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spelling ftunivnebraskali:oai:digitalcommons.unl.edu:diffendal-1051 2023-11-12T04:13:34+01:00 Geology of the Ponca Creek and Keya Paha River Drainage Basins in Nebraska Diffendal, Robert F., Jr. 1997-09-01T07:00:00Z application/pdf https://digitalcommons.unl.edu/diffendal/51 https://digitalcommons.unl.edu/context/diffendal/article/1051/viewcontent/Archaeological_Survey_Ponca_Keya_Paha_Diffendal_Sep_97_REV.pdf unknown DigitalCommons@University of Nebraska - Lincoln https://digitalcommons.unl.edu/diffendal/51 https://digitalcommons.unl.edu/context/diffendal/article/1051/viewcontent/Archaeological_Survey_Ponca_Keya_Paha_Diffendal_Sep_97_REV.pdf Robert F. Diffendal, Jr., Publications Earth Sciences Geology Geomorphology Hydrology Stratigraphy text 1997 ftunivnebraskali 2023-10-30T11:31:50Z The geology of the study area has been investigated many times over more than a century. Interested readers are directed to the report by Diffendal and Voorhies (1994), which gives a more detailed overview of the results of the investigations and lists most of the more important reports about the area’s geology. The names of the sedimentary rock strata and unlithified sediments exposed in and underlying all or parts of the study area are shown in Table V.I. These formations range in age from more than 85 million years to sediments being deposited today by winds, water, and downslope movements (landslides). The oldest sedimentary rocks belonging to the Niobrara Formation and younger Pierre Shale were deposited on the floor of a seaway that connected the Gulf of Mexico with the Arctic Ocean near the end of the Cretaceous Period. The Niobrara Formation is exposed only along the lower valley sides at the downstream end of Ponca Creek in Boyd County and along the lower valley sides along the Missouri River. The Niobrara Formation consists primarily of gray to white chalks, shaley chalks, and limestones formed mainly of the microscopic limey skeletal debris from marine plants. Larger fossils of clams, oysters, cephalopods, fish, and marine reptiles occur in this formation. The Pierre Shale is composed principally of gray to black platey shales and limey shales. Sulfur-bearing minerals in the shale often yield a rotten-egg odor in the air above exposures. Neither of these formations yields significant materials for tools. Text Arctic Arctic Ocean University of Nebraska-Lincoln: DigitalCommons@UNL Arctic Arctic Ocean Rotten ENVELOPE(-53.417,-53.417,68.867,68.867)
institution Open Polar
collection University of Nebraska-Lincoln: DigitalCommons@UNL
op_collection_id ftunivnebraskali
language unknown
topic Earth Sciences
Geology
Geomorphology
Hydrology
Stratigraphy
spellingShingle Earth Sciences
Geology
Geomorphology
Hydrology
Stratigraphy
Diffendal, Robert F., Jr.
Geology of the Ponca Creek and Keya Paha River Drainage Basins in Nebraska
topic_facet Earth Sciences
Geology
Geomorphology
Hydrology
Stratigraphy
description The geology of the study area has been investigated many times over more than a century. Interested readers are directed to the report by Diffendal and Voorhies (1994), which gives a more detailed overview of the results of the investigations and lists most of the more important reports about the area’s geology. The names of the sedimentary rock strata and unlithified sediments exposed in and underlying all or parts of the study area are shown in Table V.I. These formations range in age from more than 85 million years to sediments being deposited today by winds, water, and downslope movements (landslides). The oldest sedimentary rocks belonging to the Niobrara Formation and younger Pierre Shale were deposited on the floor of a seaway that connected the Gulf of Mexico with the Arctic Ocean near the end of the Cretaceous Period. The Niobrara Formation is exposed only along the lower valley sides at the downstream end of Ponca Creek in Boyd County and along the lower valley sides along the Missouri River. The Niobrara Formation consists primarily of gray to white chalks, shaley chalks, and limestones formed mainly of the microscopic limey skeletal debris from marine plants. Larger fossils of clams, oysters, cephalopods, fish, and marine reptiles occur in this formation. The Pierre Shale is composed principally of gray to black platey shales and limey shales. Sulfur-bearing minerals in the shale often yield a rotten-egg odor in the air above exposures. Neither of these formations yields significant materials for tools.
format Text
author Diffendal, Robert F., Jr.
author_facet Diffendal, Robert F., Jr.
author_sort Diffendal, Robert F., Jr.
title Geology of the Ponca Creek and Keya Paha River Drainage Basins in Nebraska
title_short Geology of the Ponca Creek and Keya Paha River Drainage Basins in Nebraska
title_full Geology of the Ponca Creek and Keya Paha River Drainage Basins in Nebraska
title_fullStr Geology of the Ponca Creek and Keya Paha River Drainage Basins in Nebraska
title_full_unstemmed Geology of the Ponca Creek and Keya Paha River Drainage Basins in Nebraska
title_sort geology of the ponca creek and keya paha river drainage basins in nebraska
publisher DigitalCommons@University of Nebraska - Lincoln
publishDate 1997
url https://digitalcommons.unl.edu/diffendal/51
https://digitalcommons.unl.edu/context/diffendal/article/1051/viewcontent/Archaeological_Survey_Ponca_Keya_Paha_Diffendal_Sep_97_REV.pdf
long_lat ENVELOPE(-53.417,-53.417,68.867,68.867)
geographic Arctic
Arctic Ocean
Rotten
geographic_facet Arctic
Arctic Ocean
Rotten
genre Arctic
Arctic Ocean
genre_facet Arctic
Arctic Ocean
op_source Robert F. Diffendal, Jr., Publications
op_relation https://digitalcommons.unl.edu/diffendal/51
https://digitalcommons.unl.edu/context/diffendal/article/1051/viewcontent/Archaeological_Survey_Ponca_Keya_Paha_Diffendal_Sep_97_REV.pdf
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