Early and middle Bajocian (Middle Jurassic) ammonites from southern Alaska
R. W. Imlay
1984, Professional Paper 1322
No abstract available....
Simulated effects of proposed reservoir-development alternatives on streamflow quantity in the White River, Colorado and Utah
Gerhard Kuhn, S. R. Ellis
1984, Water-Resources Investigations Report 84-4297
Numerous reservoirs have been proposed for the White River basin in Colorado and Utah, primarily to provide water for oil-shale development. A multireservoir-flow model was used to simulate the effects of streamflow withdrawal at four of the proposed reservoirs using historical streamflow data from the 1932-81 water years. The proposed...
Hydrologic data for the Larimer-Weld regional water-monitoring program, Colorado, 1975-82
S. R. Blakely, J.T. Steinheimer
1984, Open-File Report 84-139
The Larimer-Weld, Colorado, regional Monitoring Program was begun in 1976 to provide information on the quality and quantity of the surface-water resources in the area. Three stations on the big Thompson River and five stations on the Cache La Poudre River were selected for a data-collection network. Four previously established...
Maps showing ground-water units and withdrawal, Basin and Range Province, Texas
B. T. Brady, M. S. Bedinger, John Mikels
1984, Water-Resources Investigations Report 83-4121-A
This report on ground-water units and withdrawal in the Basin and Range province of Texas (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing...
Corals as guides to divisions of the Pennsylvanian system in the Western Interior region
W.J. Sando
1984, Open-File Report 84-79
Palynological evaluation of Cedar Mountain and Burro Canyon formations, Colorado Plateau
R.H. Tschudy, B.D. Tschudy, L.C. Craig
1984, Professional Paper 1281
Geohydrology of the Madison and associated aquifers in parts of Montana, North Dakota, South Dakota, and Wyoming
J. S. Downey
1984, Professional Paper 1273-G
The Schultze granite, the Tea Cup granodiorite, and the Granite Basin porphyry: A geochemical comparison of mineralized and unmineralized stocks in southern Arizona
S.C. Creasey
1984, Professional Paper 1303
No abstract available....
Surficial geology of the west half of the Skykomish River Quadrangle, Snohomish and King counties, Washington
D. B. Booth
1984, Open-File Report 84-213
Syringoporoid corals; guides to the stratigraphy of upper Paleozoic rocks in the Western Interior region
W.J. Sando
1984, Open-File Report 84-80
The thrust belt in Southwest Montana and east-central Idaho
Edward T. Ruppel, David A. Lopez
1984, Professional Paper 1278
The leading edge of the Cordilleran fold and thrust in southwest Montana appears to be a continuation of the edge of the Wyoming thrust belt, projected northward beneath the Snake River Plain. Trces of the thrust faults that form the leading edge of the thrust belts are mostly concealed, but...
Downstream effects of dams on alluvial rivers
G. P. Williams, M. G. Wolman
1984, Professional Paper 1286
Stratigraphy and sedimentary facies of the Madison Limestone and associated rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming
J.A. Peterson
1984, Professional Paper 1273-A
Reconnaissance geology of the Wadi Habawnah Quadrangle, sheet 17/44 A, Kingdom of Saudi Arabia
E.G. Sable
1984, Open-File Report 84-326
Igneous activity and related ore deposits in the western and southern Tushar Mountains, Marysvale volcanic field, west-central Utah
Thomas A. Steven, editor(s)
1984, Professional Paper 1299-A,B
PART A: Igneous activity in the Marysvale volcanic field of western Utah can be separated into many episodes of extrusion, intrusion, and hydrothermal activity. The rocks of the western Tushar Mountains, near the western part of the volcanic field, include intermediate-composition, calc-alkalic volcanic rocks erupted from scattered volcanoes in Oligocene...
Batholithic rocks of Southern California: A model for the petrochemical nature of their source materials
A. K. Baird, A.T. Miesch
1984, Professional Paper 1284
No abstract available....
Statistical relations among earthquake magnitude, surface rupture length, and surface fault displacement
M. G. Bonilla, R. K. Mark, J. J. Lienkaemper
1984, Open-File Report 84-256
In order to refine correlations of surface-wave magnitude, fault rupture length at the ground surface, and fault displacement at the surface by including the uncertainties in these variables, the existing data were critically reviewed and a new data base was compiled. Earthquake magnitudes were redetermined as necessary to make them...
Definition of boundary and initial conditions in the analysis of saturated ground-water flow systems; an introduction
O.L. Franke, T. E. Reilly, G.D. Bennett
1984, Open-File Report 84-458
Accurate definition of boundary and initial conditions is an essential part of conceptualizing and modeling ground-water flow systems. This report explains the properties of the seven most common boundary conditions encountered in ground-water systems and discusses major aspects of their application. It also discusses the significance and specification of initial...
Maps showing ground water levels, springs, and depth to water, Basin and Range Province, Arizona
W. H. Langer, D. A. Mulvihill, T. W. Anderson
1984, Water-Resources Investigations Report 83-4114-B
No abstract available....
The Richmond and Greenwich slices of the Hamburg klippe in eastern Pennsylvania — Stratigraphy, sedimentology, structure, and plate tectonic implications
G. G. Lash, Avery A. Drake Jr.
1984, Professional Paper 1312
No abstract available....
Utilization of surface coal mine wastewater for construction of a northern pike spawning/rearing marsh
Richard W. Gregory, Allen A. Elser, Thomas Lenhart
1984, FWS/OBS 84/03
An evaluation of rainfall-runoff data for the Denver Federal Center, Lakewood, Jefferson County, Colorado
R.D. Jarrett, J.E. Veenhuis
1984, Water-Resources Investigations Report 84-4050
An investigation was made to monitor the storm runoff in McIntyre Gulch basin to determine the rainfall-runoff chracteristics. Results may now be used to evaluate the effects of future development on storm runoff from the Denver Federal Center, which is located in the McIntyre Gulch basin in Lakewood , CO....
Chemical data for soils over and around the Velma oil field, Stephens County, Oklahoma
S.S. Roeming, T.J. Donovan
1984, Open-File Report 84-262
Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age
G. W. Leo, R. E. Zartman, D. G. Brookins
1984, Professional Paper 1295
The Glastonbury dome is a long, narrow structure trending approximately 70 km north-northeast through Connecticut and Massachusetts along the west side of the Bronson Hill anticlinorium. Structurally and stratigraphically the dome is analogous to the Oliverian domes of New Hampshire. It is cored by Glastonbury Gneiss and is mantled by...
Hydrologic effects of impoundments in Sherburne National Wildlife Refuge, Minnesota
R. G. Brown
1984, Water-Resources Investigations Report 84-4175
The hydrologic effects of proposed impoundments in Sherburne National Wildlife Refuge were found to be insignificant with respect to both ground- and surface-water flow patterns and water quality. Monitoring of water levels in 23 observation wells and of discharge in the St. Francis River during 1980 and 1981 has shown...