Ground-water resources of alluvial valleys in northeastern Puerto Rico

Río Espíritu Santo to Río Demajagua area by Francisco PГ©rez-Blair

Publisher: U.S. Dept. of the Interior, U.S. Geological Survey, Publisher: Branch of Information Services [distributor] in San Juan, P.R, Denver, CO

Written in English
Published: Pages: 25 Downloads: 45
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Subjects:

  • Groundwater -- Puerto Rico -- Espíritu Santo River,
  • Groundwater -- Puerto Rico -- Demajagua River

Edition Notes

Other titlesGround water resources of alluvial valleys in northeastern Puerto Rico, Río Espíritu Santo to Río Demajagua area
Statementby Francisco Pérez-Blair ; prepared in cooperation with the Puerto Rico Aqueduct and Sewer District
SeriesWater-resources investigations report -- 96-4201
ContributionsPuerto Rico Aqueduct and Sewer Authority, Geological Survey (U.S.)
The Physical Object
Paginationv, 25 p. :
Number of Pages25
ID Numbers
Open LibraryOL13620784M
OCLC/WorldCa37207833

Texas Water Development Board. North Congress Avenue, Austin, TX TEL: / FAX: Footer Social Media Navigation. As previously stated in the discussion of how alluvial aquifers form, this is definitely not the case. Additionally, the boundaries for the geology map are based largely on the Geologic Map of Kansas of The alluvial deposits in this shapefile are separated into Tertiary, Kansan and post-Kansan deposits. Ground Water Bulletin # Hydrogeology of the Principal Aquifers in Vigo & Clay Counties () () Hydrogeology of the Principal Aquifers in Vigo and Clay Counties, Indiana. Interpretive report by L. W. Cable, F. A. Watkins, Jr., and T. M. Robison about ground-water resources of Vigo and Clay Counties. GEOLOGY AND WATER RESOURCES OF THE SPANISH VALLEY AREA, GRAND AND SAN JUAN COUNTIES, UTAH by C. T. Sumsion Hydrologist, U. S. Geological Survey ABSTRACT The Spanish Valley area covers about square miles on the western slopes of the La Sal Mountains in southeastern Utah; within it, Spanish Valley comprises about 18 square by:

Water levels were measured in about wells in the Mississippi River valley alluvial aquifer in northwestern Mississippi during April Ground-water levels have declined in some areas in recent years as a result of heavy irrigation pumpage from this aquifer. Near the areas of principal recharge, along the major rivers, and near the Bluff Hills, ground-water levels appear to be . Search Tips. Phrase Searching You can use double quotes to search for a series of words in a particular order. For example, "World war II" (with quotes) will give more precise results than World war II (without quotes). Wildcard Searching If you want to search for multiple variations of a word, you can substitute a special symbol (called a "wildcard") for one or more letters. Geology of Puerto Rico. Geologic units and faults from USGS Open File Report , concerning assessment of the mineral resources of Puerto Rico. Info: Geology of the conterminous United States. A digital version of the Geologic Map of the United States, originally published at a scale of ,, (King and Beikman, b). sippi and Missouri rivers where they store enormous quantities of ground-water. Thinner, narrower alluvial aquifers along major interior rivers may be from 30 to 70 feet thick. A few deposits of very thick alluvium are found where modern river valleys coincide with older, deeper, buried valleys cut into the underlying bedrock Size: 2MB.

Grossman, I.G., , Fluctuations of ground-water levels in Puerto Rico resulting from earthquakes (): 3rd Caribbean Geological Conference (Jamaica, April ) Transactions, p. Jamaica Geological Survey Publication poisoning ground water. In the northern limestone, rural populations dispose all sewage directly into the natural environment. The karst is vital to Puerto Rico because its natural resources and environ-mental conditions provide essential services to the rest of the island, including sustaining quality of life and a prosperous economy. Water. MAIN LIBRARY. Perry-Castañeda Library East 21st St. Austin, TX. Phone: () Surface-Water, Water-Quality, and Ground-Water Assessment of the Municipio of Caguas, Puerto Rico, By Fernando Gomez-Gomez, Jesus Rodrfguez-Martmez, Luis Santiago-Rivera, Mario L Oliveras-Feliciano, and Carlos Conde-Costas Water-Resources Investigations Report Prepared in cooperation with the MUNICIPIO AUTONOMO DE CAGUAS.

Ground-water resources of alluvial valleys in northeastern Puerto Rico by Francisco PГ©rez-Blair Download PDF EPUB FB2

Get this from a library. Ground-water resources of alluvial valleys in northeastern Puerto Rico: Río Espíritu Santo to Río Demajagua area.

[Francisco Pérez-Blair; Puerto Rico Aqueduct and Sewer Authority.; Geological Survey (U.S.)]. Ground-Water Resources of Alluvial Valleys in Northeastern Puerto Rico - Rfo Espiritu Santo to Rio Demajagua Area By Francisco Perez-Blair Abstract A ground-water resources assessment was conducted in several alluvial valley aquifers associated with the principal streams in an area of about square kilometers in northeastern Puerto by: 3.

Pérez-Blair F. Ground Water Resources of Alluvial Valleys in Northeastern Puerto Rico—Río Espíritu Santo to Río Demajaua Area. United States Geological Survey Water Resources Investigations Report San Juan, PR. In article [25] Puerto Rico Department of Health.

Cited by: 1. GROUND WATER ATLAS of the UNITED STATES Alaska, Hawaii, Puerto Rico and the U. Virgin Islands HA N Preview and download Puerto Rico and the U.

Virgin Islands Alluvial valley aquifers figures--(80 thru 86) Download the text (This is the text for all of HA N in ascii format, no links, no page formatting) --(60k). Puig, J. and Rodríguez-Martínez, J. Ground-water resources of the Caguas-Juncos Valley, Puerto Rico. U.S. Geological Survey.

Water-Resources Investigations Report Quiñones-Aponte, V., Simulation of ground-water flow. Pé-Blair, F. () Ground-water Resources of Alluvial Valleys in Northeastern Puerto Rico—Rí Espí Santo to Rí Demajagua Area.

Water Resources Investigations Report 96. GROUND WATER OPERATIONAL MODEL YAUCO, PUERTO RICO PREPARED BY: Tanca St. P.O. Box. Old San Juan Tel. () Fax.

() PREPARED FOR: June, 0 5 10 15 20 25 30 35 40 45 50 55 60 65 70 75 80 0 5 10 15 20 25 30 35 40 45 50 55 60File Size: 4MB. The processing steps are discussed separately for Puerto Rico, and the Virgin Islands PUERTO RICO *Aquifer contact lines The aquifer contact information was originally compiled by Robert A.

Renken at a scale ofon scale-stable material. The contacts were scribed at a lineweight of ". This atlas presents an overview of the ground-water resources of the main island of Puerto Rico; two of its larger offshore islands, Isla de Culebra and Isla de Vieques; and the three principal islands of the U.S.

Virgin Islands, St. Thomas, St. John, and St. Croix. The atlas presents the most important ground-water information available for these islands, and is written for water. The study area is located on the north coast of Puerto Rico, in the Municipality of Grande de Manati.

The extent of the alluvial deposits within the study area was 21. A synoptic survey of the hydrologic conditions in the Río Nigua de Salinas alluvial fan was conducted from July 9 to 11,to define the spatial distribution of the potentiometric surface. The survey was part of a major study to assess the ground-water quality in the Río Nigua de Salinas alluvial aquifer.

The Río Nigua de Salinas alluvial fan covers approximately 9. GEOLOGY AND GROUND-WATER RESOURCES OF NORTHEASTERN SOCORRO COUNTY, NEW MEXICO. BY ZANE SPIEGEL. Geological Survey. Abstract. This report presents the results of an investigation of the ground-water conditions and resources in northeastern Socorro County made by the United States Geological Survey in cooperation with the New Mexico.

GROUND WATER POLLUTION IN ARIZONA, CALIFORNIA, NEVADA & UTAH by Dean K. Fuhriman and James R. Barton FUHRIMAN, BARTON 6 ASSOCIATES Provo, Utah for the OFFICE OF RESEARCH AND MONITORING ENVIRONMENTAL PROTECTION AGENCY PROJECT #ERU CONTRACT # Deceirtoer, For sale by the.

Three-dimensional ground-water-flow model of the water-table aquifer in Vega Alta, Puerto Rico [Sepúlveda, Nicasio.] on *FREE* shipping on qualifying offers. Three-dimensional ground-water-flow model of the water-table aquifer in Vega Alta, Puerto RicoAuthor: Nicasio.

Sepúlveda. The Geology of Pennsylvania consists of six distinct physiographic provinces, three of which are subdivided into different sections. Each province has its own economic advantages and geologic hazards and plays an important role in shaping everyday life in the state.

They are: (listed from the southeast corner to the northwest corner) the Atlantic Coastal Plain Province, the. Bennett, G.D.,Ground water along Río Bucaná at Ponce, Puerto Rico and the effects of a proposed floodway on ground-water quality, U.S.

Geological Survey Water-Resources Bulle 29 p. Bennett, G.D.,Electrical analog simulation of the aquifers along the south coast of Puerto Rico, U.S. Geological Survey Open-File Report PB EPA/// February HANDBOOK OF SUGGESTED PRACTICES FOR THE DESIGN AND INSTALLATION OF GROUND-WATER MONITORING WELLS by Linda Aller, Truman W.

Bennett and Glen Hackett Bennett & Williams, Inc. Columbus, Ohio and Rebecca J. Petty Ohio Department of Natural Resources Division of Ground. WSP / Swenson, F. / GEOLOGY AND GROUND-WATER RESOURCES OF THE MISSOURI RIVER VALLEY IN NORTHEASTERN MONTANA,pb, pages, 18 figs., 9 tables, 1 plate in 2 parts (in pocket), $ 32 WSP / Swenson, F.

/ GEOLOGY AND GROUND-WATER RESOURCES OF THE MISSOURI RIVER VALLEY IN NORTHEASTERN. Geology and ground-water resources of the upper Lodgepole Creek drainage basin, Wyoming, by L.J.

Bjorklund, with a section on Chemical quality of the water, by R.A. Krieger and E.R. Jochens. 40 p. 2 pl. [Note—Geology and ground-water resources of the lower Lodgepole Creek drainage basin, Nebraska, are described in WSP ]. Abstract. Subsurface data and results of surface geologic mapping indicate that areal variations in hydraulic conductivity of water-bearing strata in the semiarid alluvial plain of southern Puerto Rico may be controlled by geologic structure and depositional by: 4.

Alluvial deposits are sediments composed of gravel, sand, silt or clay deposited in river channels or on floodplains. They occur in most regions of Australia and are a major resource for irrigation, town, stock and domestic uses.

Ground water resources of the Bryce Canyon National Park area, Aggradation and degradation of alluvial sand deposits, toColorado River, Characterization of surface-water resources in the Great Basin National Park area and their susceptibility to ground-water withdrawals in adjacent valleys, White Pine County, Nevada (USGS.

Evaluating the ground-water resources of the High Plains of Texas, basic data for northern third of region Texas Department of Water Resources Final Report LP, v. 2, p. Evaluating the ground-water resources of the High Plains of Texas Texas Department of Water Resources Final Report LP, v.

1, p. Kolm, K.E., and Case, H.L., III. The area is characterized by north- to northwest-trending mountains separated by alluvial basins that form a regional topography of alternating mountains and valleys.

On the basis of ground-water divides or zones of minimal basin interconnection, the area was divided into 72 basins, each representing an individual aquifer : Frederick N. Robertson. The alluvial aquifers beneath the floodplains of the Mississippi and Missouri rivers are some of Missouri's most valued water resources.

These aquifers are capable of yielding from to more than 2, gallons of water per minute to properly designed and developed wells, and are widely used for municipal water supply and agricultural irrigation. Quinones-Aponte V.

Water resources of the lower Rio Grande de Arecibo alluvial valley, Puerto Rico. U.S. Geological Survey Water-Resources Investigations Report [ Google Scholar ] Renken RA, Ward WC, Gill IP, Gómez GF, Rodríguez JM, et al. Geology and hydrogeology of the Caribbean Islands aquifer system of the commonwealth of Cited by: 5.

IDENTIFICATION OF ALLUVIAL VALLEY FLOORS IN STRIPPABLE COAL AREAS OF NEW MEXICO Report to Emery Arnold, Director Mining and Minerals Division Energy and Minerals Department Santa Fe, New Mexico BY D.W.

Love and 3.W. Hawley New Mexico Bureau of Mines and Mineral Resources New Mexico Institute of Mining and Technology Socorro, New Mexico. Water resources management challenges. Management of water resources in Guatemala is shared by several government agencies and institutions.

Most of these agencies conduct their work with little or no coordination with other agencies, which creates duplication of work and inefficient use of resources. In addition, there is a need for the enactment of watershed Groundwater recharge: km³.

The Andean region is characterized by important intramontane alluvial and glacial valleys; a typical example is the Tarqui alluvial plain, Ecuador. Such valley plains are densely populated and/or very attractive for urban and infrastructural by: Ground-water resources of alluvial valleys in northeastern Puerto Rico: Río Espíritu Santo to Río Demajagua area / (San Juan, P.R.: U.S.

Dept. of the Interior, U.S. Geological Survey ; Denver, CO: Branch of Information Services [distributor], ), by Francisco Pérez-Blair, Geological Survey (U.S.), and Puerto Rico Aqueduct and Sewer.

The last assessment of ground water was carried out as on According to this assessment, net ground water resources of Punjab State are BCM, whereas net draft was BCM, leading to ground water deficit of BCM. The stage of ground water development for the State was % andFile Size: KB.H.R.

the Ground Water Research, Development and Demonstration Act, and H.R. the National Ground Water Contamination Information Act of [microform]: hearing before the Subcommittee on Natural Resources, Agriculture Research, and Environment of the Committee on Science, Space, and Technology, U.S.

House of Representatives, One.Abstract [1] In surface-water-irrigated western valleys, groundwater discharge from excess irrigation sustains winter streamflow at levels that exceed natural flows.

This unnatural condition has persisted for so long that hydrologists, water managers, and water users consider it to be normal. Changing land uses and irrigation practices complicate efforts to manage groundwater .