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Articles 1 - 22 of 22
Full-Text Articles in Stratigraphy
Groundwater Levels In Nebraska, 1975, Michael J. Ellis, Darryll T. Pederson
Groundwater Levels In Nebraska, 1975, Michael J. Ellis, Darryll T. Pederson
Conservation and Survey Division: Faculty and Staff Publications
No abstract provided.
Long-Distance Turbidite Correlations In The Horseshoe Abyssal Plain, William H. Hoyt
Long-Distance Turbidite Correlations In The Horseshoe Abyssal Plain, William H. Hoyt
Geology Theses and Dissertations
Few studies on modern abyssal plain turbidites have attempted to assess the lateral extent of individual units and few have therefore been able to provide any information on the evolution of turbidity deposits across long abyssal plain distances. In the 4755 m-deep Horseshoe Abyssal Plain, ten distinct lithologic units (six of these Iberian Peninsula-derived turbidites) were delineated in nine piston cores on the basis of stratigraphic position, thickness (range of 20 cm to greater than 500 cm), color, sediment type, sedimentary structures, x-ray mineralogy, and the ubiquitous presence of units in all abyssal plain and supplying canyon piston cores. In …
Nebraska Remote Sensing Center News, Rex Peterson, Paul Seevers
Nebraska Remote Sensing Center News, Rex Peterson, Paul Seevers
Conservation and Survey Division: Faculty and Staff Publications
No abstract provided.
Big Springs Ne Quadrangle, Garden And Deuel Counties, Nebraska, Robert F. Diffendal Jr.
Big Springs Ne Quadrangle, Garden And Deuel Counties, Nebraska, Robert F. Diffendal Jr.
Robert F. Diffendal, Jr., Publications
7.5' topgraphic quadrangle showing exposures of bedrock formations and other geologic information.
41° 07'30" — 41° 15'
102° 00' — 102° 07'30"
Scale 1:24,000
Completed July 16, 1976
High resolution .tif file attached below as supplemental file
Ruthton Quadrangle, Nebraska—Garden And Keith Counties, 7.5 Minute Series (Topographic), Robert F. Diffendal Jr.
Ruthton Quadrangle, Nebraska—Garden And Keith Counties, 7.5 Minute Series (Topographic), Robert F. Diffendal Jr.
Robert F. Diffendal, Jr., Publications
Ruthton Quadrangle, Nebraska—Garden and Keith Counties
7.5 minute series (topographic), scale 1:24000
103°07'30" to 103°15'
41°15' to 41°22'30"
Ql=loess, Qsa=sand; Ogallala & Post-Ogallala Gravels (Blancan?), Ogallala Outcrop; Pre-Ogallala Outcrop (Brule), Faunal site
July 16, 1976
Lewellen Quadrangle, Nebraska--Garden County, 7.5 Minute Series (Topographic), Robert F. Diffendal Jr.
Lewellen Quadrangle, Nebraska--Garden County, 7.5 Minute Series (Topographic), Robert F. Diffendal Jr.
Robert F. Diffendal, Jr., Publications
Lewellen Quadrangle, Nebraska--Garden County
7.5 minute series (topographic), scale 1:24,000
102°07'30" to 102°15'
41°22'30" to 41°15'
Ql = loess
Qsa = sand
Volcanic ash
Ogallala and post-Ogallala gravels
Ogallala Outcrop
Pre-Ogallala Outcrop (Brule)
Faunal site
Completed July 16, 1976
Keystone Quadrangle, Keith County, Nebraska, Robert F. Diffendal Jr.
Keystone Quadrangle, Keith County, Nebraska, Robert F. Diffendal Jr.
Robert F. Diffendal, Jr., Publications
7.5' topgraphic quadrangle showing exposures of bedrock formations and other geologic information.
41° 07'30" to 41° 15'
101° 30' to 101° 37'30"
Scale 1:24,000
Completed July 16, 1976
High resolution .tif file (130 MB) attached below as supplemental file
Physiography, Geology, And Water Resources Of Boyd County, Nebraska, Vernon L. Souders
Physiography, Geology, And Water Resources Of Boyd County, Nebraska, Vernon L. Souders
Conservation and Survey Division: Faculty and Staff Publications
No abstract provided.
Big Springs Nw Quadrangle, Garden And Deuel Counties, Nebraska, Robert F. Diffendal Jr.
Big Springs Nw Quadrangle, Garden And Deuel Counties, Nebraska, Robert F. Diffendal Jr.
Robert F. Diffendal, Jr., Publications
7.5' topgraphic quadrangle showing exposures of bedrock formations and other geologic information.
41° 07'30" — 41° 15'
102° 07'30" — 102° 15'
Scale 1:24,000
Completed July 16, 1976
High resolution .tif file attached below as supplemental file
Laws, Rules, And Regulations Pertaining To Groundwater In Nebraska, Gerald R. Svoboda
Laws, Rules, And Regulations Pertaining To Groundwater In Nebraska, Gerald R. Svoboda
Conservation and Survey Division: Faculty and Staff Publications
This publication contains (1) Nebraska laws pertaining to groundwater, and (2) the duties assigned to or the rules and regulations developed by various Nebraska agencies charged with the regulation of groundwater use. Following public hearings, rules and regulations can be changed at any time by state agencies. Each state agency with responsibility for groundwater regulation is able to supply, upon request, its rules and regulations pertaining to groundwater use. Water legislation varies from state to state because of differences in climate, availability and utilization of water, and fundamental legal concepts inherited at the time of statehood. Some states have laws …
The Geology Of The Castle Rock Area, Grant, Harney And Malheur Counties, Oregon, John David Wood
The Geology Of The Castle Rock Area, Grant, Harney And Malheur Counties, Oregon, John David Wood
Dissertations and Theses
The geology of the Castle Rock area aids in the understanding of Cenozoic volcanic stratigraphy and structures in an area where these volcanic rocks thin near the margins of the pre-Tertiary basement rocks and structural trends are overlapping. The Castle Rock area is unique in several aspects and is important in understanding and interpreting the geology in adjacent regions which have all been studied, at least on a regional basis. Intrusive ash-flow bodies of the Dinner Creek Ash-Flow Tuff, well-exposed sections of complexly interstratified volcanic rocks and well-exposed faults, and of high amount of erosional relief are features which make …
Geology And Ore Deposits Of The Johnnie District, Nye County, Nevada, Stanley Wayne Ivosevic
Geology And Ore Deposits Of The Johnnie District, Nye County, Nevada, Stanley Wayne Ivosevic
UNLV Theses, Dissertations, Professional Papers, and Capstones
The Johnnie district, in the northwestern Spring Mountains, Nye County, Nevada, may have produced a little under 100,000 troy oz of gold, since the discovery of the district in 1890.
An approximately 13,000-ft-thick (4,000 m) section of east-dipping upper Precambrian through Middle Cambrian miogeosynclinal clastic and carbonate rocks is exposed in the district. The strata are, in order of decreasing age, the Johnnie Formation, Stirling Quartzite, Wood Canyon Formation, Zabriskie Quartzite, and Carrara and Bonanza King Formations. These are overlain by Cenozoic units which include and older unit and a younger unit of fanglomerate, the older containing a megabreccia deposit, …
Water Resources Of Pierce County, Nebraska, Robert E. Brogden, Richard A. Engberg
Water Resources Of Pierce County, Nebraska, Robert E. Brogden, Richard A. Engberg
Conservation and Survey Division: Faculty and Staff Publications
No abstract provided.
Regional Tectonics And Seismicity Of Eastern Nebraska, Annual Report June 1, 1976- June 1, 1977, R. R. Burchett
Regional Tectonics And Seismicity Of Eastern Nebraska, Annual Report June 1, 1976- June 1, 1977, R. R. Burchett
Conservation and Survey Division: Faculty and Staff Publications
No abstract provided.
Regional Carbonate Deposition Of The Pitkin Limestone (Chesterian): Washington And Crawford Counties, Arkansas, Robert E. Tehan
Regional Carbonate Deposition Of The Pitkin Limestone (Chesterian): Washington And Crawford Counties, Arkansas, Robert E. Tehan
Journal of the Arkansas Academy of Science
The Pitkin Limestone overlies black shale of the Fayetteville Formation and is the youngest Mississippian unit in the Paleozoic succession of northwest Arkansas. Five major fades have been delineated within the formation by apetrographic examination of samples collected from 17 measured sections: (1) oolith facies, (2) bioclast facies, (3) nodular limestone-shale facies, (4) mudstone facies, and (5) lime mud mound facies. The distribution of these facies in the Pitkin Formation suggests that Fayetteville terrigenous sedimentation was succeeded by the deposition of widespread oolith shoals and skeletal blanket sand bodies across the northern Arkansas structural platform. Sparse accumulations of lime mud …
Structural Studies In The Northern Chester Dome Of East-Central Vermont, Bruce Wallace Nesbit
Structural Studies In The Northern Chester Dome Of East-Central Vermont, Bruce Wallace Nesbit
Geology Theses and Dissertations
Rocks in the Eastern Vermont Sequence are highly metamorphosed and are said to range in age from Precambrian to Siluro-Devonian. The sequence outcrops on Keyes Mountain, about 6km Northwest of Felchville, Vermont, and an area on this mountain about 2km square was mapped in great detail.
The dominant rock type found is quartzofeldspathic gneiss, but schistose gneiss, amphibolite, quartzite and schist also occur. Most of these rocks are layered but layering has been transposed in many places and much of it is probably secondary. Layering and schistosity both dip dominantly to the north at about 25º.
A number of mesoscopic …
Nebraska Mineral Operations Review, 1975, Raymond R. Burchett, Duane A. Eversoll
Nebraska Mineral Operations Review, 1975, Raymond R. Burchett, Duane A. Eversoll
Conservation and Survey Division: Faculty and Staff Publications
During 1975, there were active in Nebraska 42 limestone quarries; 596 sand, gravel and silt or siltstone pits; 8 clay or shale pits; 22 sandstone pits; and 1 peat pit. These 669 mining operations disturbed 663 acres and restored 161 acres during the year.
Lower Mississippian Lithostratigraphy, Northern Arkansas, Walter L. Manger, Jack L. Shanks
Lower Mississippian Lithostratigraphy, Northern Arkansas, Walter L. Manger, Jack L. Shanks
Journal of the Arkansas Academy of Science
Lower Mississippian lithostratigraphic units in northern Arkansas are (ascending order) the Bachelor, St. Joe, and Boone Formations. These formations disconformably overlie Middle Ordovician to Upper Devonian strata and are overlain disconformably by Meramecan or Chesterian strata. The Bachelor Formation is generally a thin (less than 0.3 m), persistent, orthoquartzitic sandstone with common to abundant phosphatic pebbles overlain by a green silty shale. In northwestern Arkansas, the Bachelor Formation commonly lacks sandstone. The Bachelor Formation has been confused previously with the Sylamore (Upper Devonian) and older sandstone units. Although commonly regarded as a member of the Boone Formation, the St. Joe …
Algal-Bryozoan Carbonate Buildups Within The Pitkin Limestone (Mississippian-Chesterian), Northwest Arkansas, Alex T. Warmath
Algal-Bryozoan Carbonate Buildups Within The Pitkin Limestone (Mississippian-Chesterian), Northwest Arkansas, Alex T. Warmath
Journal of the Arkansas Academy of Science
More than 14 biohermal buildups have been recognized within the Pitkin Limestone (Mississippian-Chesterian) in eastern Washington and western Madison Counties, northwest Arkansas. These buildups resemble previously described algal mounds in upper Pennsylvanian strata of the Midcontinent region, but differ in their faunal and floral constituents. The mounds are composed of calcilutite with variable amounts of spar and fossil allochemical grains. Associated flanking facies consist of mixed biosparite near the core, grading outward into oosparite. A few zones of shaly, poorly washed biomicrite containing rounded clasts bearing Archimedes fragments are interbedded with the flanking mixed biosparite facies. These clasts appear to …
Nebraska Groundwater Level (Decline & Rise) And Location Of Registered Wells, 1976
Nebraska Groundwater Level (Decline & Rise) And Location Of Registered Wells, 1976
Conservation and Survey Division: Faculty and Staff Publications
No abstract provided.
Location Of Registered Irrigation Wells In Nebraska As Of 1976
Location Of Registered Irrigation Wells In Nebraska As Of 1976
Conservation and Survey Division: Faculty and Staff Publications
No abstract provided.
Water Resources Data For Nebraska Water Year 1975
Water Resources Data For Nebraska Water Year 1975
Conservation and Survey Division: Faculty and Staff Publications
No abstract provided.