Glacial geology and aquifer characteristics of the Big River area, central Rhode Island by Janet Radway Stone

Cover of: Glacial geology and aquifer characteristics of the Big River area, central Rhode Island | Janet Radway Stone

Published by U.S. Dept. of the Interior, U.S. Geological Survey in Northborough, Mass .

Written in English

Read online

Places:

  • Rhode Island,
  • Big River Region.,
  • Kent County.

Subjects:

  • Aquifers -- Rhode Island -- Big River Region.,
  • Hydrogeology -- Rhode Island -- Big River Region.,
  • Water-supply -- Rhode Island -- Kent County.

Edition Notes

Book details

Statementby Janet Radway Stone and David C. Dickerman ; prepared in cooperation with the Rhode Island Water Resources Board.
SeriesWater-resources investigations report ;, 01-4169
ContributionsDickerman, David C., Geological Survey (U.S.), Rhode Island. Water Resources Board.
Classifications
LC ClassificationsGB701 .W375 no. 01-4169
The Physical Object
Paginationiii, 12 p. ;
Number of Pages12
ID Numbers
Open LibraryOL3628342M
LC Control Number2002418086

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4 Glacial Geology and Aquifer Characteristics of the Big River Area, Central Rhode Island gneiss (Quinn, ).

The granite has undergone Paleozoic metamorphism and has a gneissic structure and texture. Although locally massive, in most places the rock is moderately foliated and compositionally layered. Glacial lakes and ice-margin positions during deglaciation, Big River area; TABLE.

Surficial materials, well-construction characteristics, and hydraulic properties determined from aquifer tests in the Big River area, Rhode Island; PLATE. Surficial Materials Map. Glacial geology and aquifer characteristics of the Big River area, central Rhode Island [electronic resource] / by Janet Radway Stone and David C.

Dickerman ; prepared in cooperation with the Rhode Island Water Resources Board. Format Online Resource Book Published. Get this from a library. Glacial geology and aquifer characteristics of the Big River area, central Rhode Island.

[Janet Radway Stone; David C Dickerman; Geological Survey (U.S.); Rhode Island. Glacial geology and aquifer characteristics of the Big River area Water Resources Board.]. The Rhode Island Department of Environmental Management's Environmental Resource Map provides a large amount of information on Rhode Island's geology and natural resources, including: Bedrock geology and glacial deposits Hazards - floodplain mapping, stormwater areas, and coastal inundation projections Water resources Waste management Soils The map allows.

Glacial Geology: Ice sheets and landforms, Second Edition has been thoroughly revised and updated throughout and provides a modern, comprehensive summary of glacial geology and geomorphology.

The book clearly outlines glacial landforms and sediments and provides the reader with the tools required to interpret glacial landscapes/5(14). The geology of Rhode Island is based on nearly one billion year old igneous crystalline basement rocks formed as part of the microcontinent Avalonia that collided central Rhode Island book the supercontinent region experienced substantial folding associated with its landlocked position during the Alleghanian orogeny mountain building event.

The region accumulated sedimentary. Book/Printed Material Geologic framework, structure, and hydrogeologic characteristics of the Knippa Gap area in Geologic framework, structure, and hydrogeologic characteristics of the Knippa Gap area in eastern Uvalde and western Medina Counties, Texas / Glacial geology and aquifer characteristics of the Big River area, central Rhode.

Glacial River Warren, also known as River Warren, was a prehistoric river that drained Lake Agassiz in central North America between ab BP calibrated (11, and 9, 14 C uncalibrated) years ago.

A part of the uppermost portion of the river channel was designated a National Natural Landmark in Glacial geology and aquifer characteristics of the Big River area, central Rhode Island / Includes bibliographical references. Also available via the World Wide Web. Also available via. A huge amount of water exists in the ground below your feet, and people all over the world make great use of it.

But it is only found in usable quantities in certain places underground — aquifers. Read on to understand the concepts of aquifers and how water exists in the ground. A hole dug at the beach is a great way to illustrate the concept.

Aquifers: Ground Water Atlas of the United States. The Ground Water Atlas of the United States, USGS Hydrologic Atlas (Miller, ), describes the location, hydrologic characteristics, and geologic characteristics of the principal aquifers throughout the 50 States, Puerto Rico, and the U.S.

Virgin groundwater information summarized in the Atlas was collected over. Geological History of Jamestown, Rhode Island. Glaciation. Many of the most notable features of the Narragansett Bay region were formed during a period of repeated glacial formation and withdrawal known as the Pleistocene Epoch.

The southern Rhode Island coastal lagoons were formed after the retreat of the Laurentide Ice Sheet at the end of the last glaciation. The Laurentide Ice Sheet extended south to Nantucket, MA, Block Island, RI, and Long Island, NY, ab to 30, years ago (CRMC ).

At that time, with so much water locked upCited by: 1. Rhode Island Rivers Shown on the Map: Blackstone River, Branch River, Pawcatuck River, Pawtuxet River, Ponaganset River, Providence River, Sakonnet River, Usquepaug River, Wood River and Woonasquatucket River.

Rhode Island Lakes Shown on the Map: Flat River Reservoir, Mt. Hope Bay, Narragansett Bay, Pascoag Lake, Scituate Reservoir, Smith and Sayles. The lack of radiocarbon ages and correlated varve sequences in southeastern New England has left the deglacial chronology of the region poorly constrained.

A year varve series from Glacial Lake Narragansett was constructed from eight continuous sediment cores collected from the Providence River, Narragansett Bay, Rhode Island. This varve series could Cited by: 1. Field Guides to the Quaternary Geology of Central Idaho: Part A.

Glacial Deposits of the Big Wood River Valley Suzanne Pearce1 Gunnar Schliederl Edward B. Evensonl INTRODUCTION Detailed mapping indicates that the Big Wood River drainage preserves the deposits of at least two Quaternary glaciations. The Genesee River, flowing into this lake carrying large amounts of silt from the area to the south, formed a delta.

Today the town of Irondequoit covers much of this delta. The western part of it extends west of Lake Avenue, and Charlotte High School stands near the edge of the delta.

The U.S. Geological Survey (USGS) and the National Oceanic and Atmospheric Administration (NOAA) are working together to study sea-floor environments off the northeast coast of the United States.

DuringNOAA survey H collected multibeam echosounder data in a square kilometer area in central Rhode Island Sound, southeast of Point Judith, Rhode Island. Rhode Island is a tucked-away little state on the coast of New England, but its small size belies beautiful scenery and terrain full of dramatic stories of geologic history.

Whether you’re relaxing harborside in Newport, tooling around on country roads or hiking in a nature preserve, Rhode Island’s landscape rewards a.

A bucket full of glacial till would have a greater mix of particle sizes. It may have cobbles and pebbles mixed in with the sand, silt and clay.

Some of the larger glacial till cobbles may even have scratches or grooves that were created when the glacier was grinding the rocks together. River rocks would not show that type of scratching. Rhode Island consists of acidic crystalline rocks including granite, gneiss, granodiorite, and shist.

The gray area on the map to the left shows the general area covered by the Narragansett Basin. PARENT MATERIALS Glacial tills and glacial outwash deposits are the two most common parent material types in Rhode Island. Till can be either subglacial.

Rhode Island geologic map data A GIS database of geologic units and structural features in Rhode Island, with lithology, age, data structure, and. Rhode Island is in the Atlantic Ocean Watershed. Most of the state's streams drain into Narragansett Bay or into the Pawcatuck River.

Most of these lakes and streams can be clearly seen on the Rhode Island Satellite Image. We also have a page about Rhode Island water resources.

Rhode Island Elevation Map: This is a generalized topographic map. Long Island’s “basement” bedrock is to million years old and is made of metamorphic rock (Merguerian and Sanders 4).

The upper portion of Long Island’s geological layers were formed between the Upper Cretaceous Period (72 to million years ago) and Pleistocene Epoch to million years ago), and consists of mostly. Geologic unit mapped in Massachusetts: Sandstone, graywacke, shale and conglomerate; minor beds of meta-anthracite.

Fossil plants. Rhode Island Formation is thickest and most extensive formation in Narragansett basin. Does not extend to Norfolk basin. Consists of gray sandstone and siltstone and lesser amounts of gray to black shale, gray conglomerate, and coal beds 10.

The formation and movement of sediments in glacial environments is shown diagrammatically in Figure There are many types of glacial sediment generally classified by whether they are transported on, within, or beneath the glacial ice.

The main types of sediment in a glacial environment are described : Steven Earle. Notice - The USGS Water Resources Mission Area's priority is to maintain the safety and well-being of our communities, including providing critical situational awareness in times of flooding in all 50 U.S.

states and additional territories. Our hydrologic monitoring stations continue to send data in near real-time to NWISWeb, and we are continuing critical water monitoring activities to. The purpose of this guidebook is to provide conference participants with an up-to-date general summary of the glacial geology of central Minnesota and a comprehensive reference list of previous research completed in the area.

There are a number of reasons why we were motivated to host the Friends of the Pleistocene in central : A.R. Knaeble. vector digital data Hartford, Connecticut, USA State of Connecticut, Department of Environmental Protection Connecticut Surficial Aquifer Texture is a derivative data product of the ,scale Connecticut Surficial Materials data.

Connecticut Surficial Materials was digitized from ,scale compilation sheets used to prepare and publish a ,scale statewide map.

Reviews the geological processes that shaped Jamestown, Rhode Island, the Narragansett Bay area, New England and North America. Starts with the formation of Avalonia about million years ago, continues through continental collisions, glacial modifications to the land and post-glacial increases in sea level.

A Prelude covers the first 4 billion years of continental formation. The photograph to the right shows a particularly nice example of shoestring topography. In this case, the sedimentary rocks formed from the sediment of a former river have proved more resistant to erosion than the rocks of its former floodplain, and so the former river stands clear as a ridge of sedimentary rock of different composition from that of the surrounding landscape.

CHAPTER 2: RHODE ISLAND’S FISH AND WILDLIFE HABITAT Geology The geologic history of Rhode Island includes two periods of mountain-building followed by extensive periods of erosion that produced the state’s current lowland and gently rolling topography (Gibbs et al. ; Quinn ). The fault lines produced by Rhode Island’sFile Size: 1MB.

I. Index of publications bearing upon the geology and mineralogy of Rhode Island, chronologically arranged. -- II. Catalogue of rocks, minerals and soils, collected during the Geological survey of Rhode Island, summer ofby Charles T. Jackson. -- III. Catalogue of fossils found in Rhode Island.

-- IV. Catalogue of minerals found in Rhode Pages: Most of the papers in this thematic section present regional perspectives that build on more than years of geologic investigation in Long Island Sound. When viewed collectively, a common theme emerges in these works.

The major geologic components of the Long Island Sound basin (bedrock, buried coastal-plain strata, recessional moraines, glacial-lake deposits, and the. WSP / Nichols, W.

/ SIMULATION ANALYSIS OF THE UNCONFINED AQUIFER, RAFT RIVER GEOTHERMAL AREA, IDAHO-UTAH,pb, 46 pages, 13 figs., 7 tables, $ 5 WSP / Knott, J. / RECONNAISSANCE ASSESSMENT OF EROSIN AND SEDIMENTATION IN THE CAÑADA DE LOS ALAMOS BASIN, LOS ANGELES AND VENTURA COUNTIES. Big River Basin Geology.

KRIS Web Background Pages: Geology. Note: Geologic information, electronic maps and models within KRIS projects are meant to provide background information only and not as a decision making rnia requires that licensed geologists be involved directly in decisions related to geologic conditions (see requirement).

Geologic Framework and Glaciation of the Central Area Christopher L. Hill The glacial geology of the central region of North America includes evidence of the lobes (Hare Indian River phase), while glacial Lake Mackenzie expanded southward as the ice front melted.

To the south. VOLCANIC ROCKS IN THE NARRAGANSETT BASIN, SOUTHEASTERN NEW ENGLAND: PETROLOGY AND SIGNIFICANCE TO EARLY BASIN FORMATION ANTON MARIA* and O. DON HERMES Department of Geosciences, University of Rhode Island, Kingston, Rhode Island, ABSTRACT. A suite of volcanic rocks in the northwest corner of the Narragansett.

The Laurentide Ice Sheet was a glacial complex that covered large portions of eastern, central and northern North America during the last glacial period. Originating on the Labrador-Ungava Plateau and on the mountains of the Arctic Islands of Canada, this glacial ice mass spread all the way down to what is now Cincinnati, Ohio.

Geology of New River Gorge. One of these glacial advances dammed the river with ice and debris at about present-day Cillicothe, Ohio, creating a large lake that backed up to the vicinity of Gauley Bridge. This caused the Teays to seek a new course skirting the edge of the glacier.

The new course was and still is the Ohio River.Sanocki, C.A.,Physical characteristics of stream subbasins in the Upper Wapsipinicon River, Upper Cedar River, Shell Rock River, and Winnebago River Basins, southern Minnesota and northern Iowa: U.S. Geological Survey Open-FileReport10 p., 1 plate.Geology and stratigraphy of the Challis Volcanic Group and related rocks, Little Wood River area, south-central Idaho: USGS Bulletin II [Sandford, Richard F., Snee, Lawrence W.] on *FREE* shipping on qualifying offers.

Geology and stratigraphy of the Challis Volcanic Group and related rocks, Little Wood River area, south-central Idaho: USGS Bulletin Author: Richard F. Sandford, Lawrence W. Snee.

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