Relevant bibliographies by topics / Geology New Hampshire

Academic literature on the topic 'Geology New Hampshire'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Geology New Hampshire"

1

Boudette, Eugene L. "The Geology of New Hampshire." Rocks & Minerals 65, no. 4 (July 1990): 306–12. http://dx.doi.org/10.1080/00357529.1990.11761687.

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Bothner, Wallace A., and Herbert Tischler. "Fossils of New Hampshire." Rocks & Minerals 65, no. 4 (July 1990): 314–20. http://dx.doi.org/10.1080/00357529.1990.11761689.

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Dallaire, Donald. "Beryllium Minerals in New Hampshire." Rocks & Minerals 97, no. 3 (April 26, 2022): 208–35. http://dx.doi.org/10.1080/00357529.2022.2028096.

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Dallaire, Donald. "Beryllium Minerals in New Hampshire." Rocks & Minerals 97, no. 3 (April 26, 2022): 208–35. http://dx.doi.org/10.1080/00357529.2022.2028096.

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Smith, Arthur E. "New Hampshire mineral locality index." Rocks & Minerals 80, no. 4 (July 2005): 242–61. http://dx.doi.org/10.3200/rmin.80.4.242-261.

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Young, James. "Fluorite Deposits of Westmoreland, New Hampshire." Rocks & Minerals 65, no. 4 (July 1990): 328–35. http://dx.doi.org/10.1080/00357529.1990.11761691.

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Thompson, Woodrow B. "History of research on glaciation in the White Mountains, New Hampshire (U.S.A.)." Géographie physique et Quaternaire 53, no. 1 (October 2, 2002): 7–24. http://dx.doi.org/10.7202/004879ar.

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Abstract The glacial geology of the White Mountains in New Hampshire has been the subject of many investigations since the 1840's. A series of controversies evolved during this period. First was the question of what geologic processes were responsible for eroding the bedrock and depositing the cover of surficial sediments. By the 1860's, the concept of glaciation replaced earlier theories invoking floods and icebergs. Research in the late 1800's concerned the relative impact of continental versus local glaciation. Some workers believed that surficial deposits in northern New Hampshire were the product of valley glaciers radiating from the White Mountains, but in the early 1900's continental glaciation was established as the most important process across the region. Debate over the extent and timing of alpine glaciation in the Presidential Range has continued until recent years. The most intensely argued topic has been the manner in which the Late Wisconsinan ice sheet withdrew from the White Mountains: whether by rapid stagnation and downwastage, or by progressive retreat of a still-active ice margin. The stagnation model became popular in the 1930's and was unchallenged until the late 1900's. Following a research hiatus lasting over 40 years, renewed interest in the glacial history of the White Mountains continues to inspire additional work.
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Thompson, Woodrow B., Alexander U. Falster, and Thomas J. Mortimer. "The Keyes Mica Mines, Orange, Grafton County, New Hampshire." Rocks & Minerals 97, no. 4 (June 28, 2022): 302–29. http://dx.doi.org/10.1080/00357529.2022.2053622.

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Bearss, Gene T., and Bob Janules. "Miarolitic Cavity Minerals of the Government PIT, Albany New Hampshire." Rocks & Minerals 67, no. 3 (June 1992): 158–68. http://dx.doi.org/10.1080/00357529.1992.9926474.

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Chamberlain, C. Page, and Philip C. England. "The Acadian Thermal History of the Merrimack Synclinorium in New Hampshire." Journal of Geology 93, no. 5 (September 1985): 593–602. http://dx.doi.org/10.1086/628983.

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Dissertations / Theses on the topic "Geology New Hampshire"

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Camp, Kristen F. "Mineralogy and Geochemistry of Anorogenic Granitic Miarolitic Pegmatites Associated with the White Mountain Intrusive Suite, New Hampshire." ScholarWorks@UNO, 2011. http://scholarworks.uno.edu/td/1363.

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Subvolcanically emplaced granitic, miarolitic pegmatites associated with the White Mountain Igneous Province (WMIP), New Hampshire, were sampled and analyzed using modern analytical techniques including X-ray fluorescence, electron microprobe, scanning electron microscopy, and direct-coupled plasma spectrophotometry. Analytical results suggest that all the sampled miarolitic pegmatites from this study are petrogenetically related to the same intrusive suite, the WMIP. Based on the geochemical data, all the samples formed in an anorogenic tectonic setting and are rift-related. They are classified as NYF-type and plot in the “within plate granite” field on tectonic discrimination diagrams. The majority of the samples are peraluminous, A1-type granites. The trace element abundances on the spider diagram and chondrite-normalized diagram, which include a pronounced negative Eu anomaly and REE enrichments, are consistent with these miarolitic pegmatites resulting from a strongly fractionated granitic parental melts, but less fractionated than the classic NYF-systems such as South Platte (Simmons et al. 1987) and the Wausau Syenite Complex (Meyers et al. 1984).
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Pett, Teresa K. "Garnetites of the Cardigan Pluton - Evidence for Restite and Implications for Source Rock Compositions." BYU ScholarsArchive, 2006. https://scholarsarchive.byu.edu/etd/1099.

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The Cardigan pluton, located in the southern half of New Hampshire, is a strongly peraluminous, S-type granite which is granodioritic in composition. It is inferred to have been emplaced rapidly, thrust up along west-verging nappes during the Acadian orogeny. Distinctive pods, consisting of 50 to 70 percent modal garnet, are found throughout the pluton in assemblages of garnet + sillimanite + biotite + plagioclase + quartz. These garnetite rocks present an intriguing case for restite. Textural features of the garnetite rocks, such as fibrolitic sillimanite mats and flat, unzoned major and trace-element garnet grain profiles, provide evidence for biotite dehydration melting with single-stage garnet growth from the reaction: bio + plag + qtz + kspar = gar + sill + liq. Temperatures calculated using garnet-biotite (GB) thermometry and garnet-aluminum silicate-quartz-plagioclase (GASP) barometry yield estimates between 662-714ºC and 3.8 kbars. These low calculated temperatures are most likely the result of biotite compositions which have been altered by retrograde exchange reactions. The dominant source rock for the Cardigan magmas was likely calc-pelitic to greywacke in composition. Major element modeling suggests that ~70% melting of a calc-pelitic metasediment from the Central Maine trough could have generated a granodioritic melt similar to the average granodiorite of the Cardigan pluton. However, most of the Cardigan garnetite rocks appear to have been derived from pelites, as they are too poor in CaO and Na2O. Hence, though the majority of garnetite rocks cannot represent the dominant restite of the source rocks that produced the Cardigan pluton, they do appear to be the melt-depleted residue of an unidentified pelitic source. Comparison of Nd and Sr isotopic data from garnetite and Central Maine trough metasediments permit an interpretation that the Lower Rangeley Formation, from the Central Maine trough, could be the source rock of the Cardigan magmas. However, one feldspar Pb isotopic analysis in the literature (Moench and Allienikoff, 2002) and rare monazite chemical ages near 600 Ma suggest that the Cardigan pluton does not have a Laurentian source (i.e. Lower Rangeley Formation or other Central Maine trough metasediments), whereas an inferred peri-Gondwanan basement source is permissible.
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Evans, Thomas Philip. "Reconciling the structural and metamorphic record of orogeny in central western New Hampshire through microstructure and garnet isopleth thermobarometry." Thesis, 2004. https://researchonline.jcu.edu.au/1188/1/01front.pdf.

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This thesis consists of four sections, each a stand-alone body of work intended for publication in international journals. The sections are ordered such that they progress in a logical fashion; the first two sections form an introduction to the new analytical techniques developed and utilised within this thesis, the remaining two sections present data and geological interpretations derived from the application of these techniques. Volume 1 contains the text and reference list, whilst Volume 2 contains the figures and appendices. Section A describes the technique of garnet isopleth thermobarometry, and outlines methods for analysing the relative contributions of the sources of error inherent to this technique. Additionally, some insights into the significance of common compositional variations within garnet are provided and discussed. Section B describes a method for calculating the changes in composition of the chemical system from which garnet is growing that are caused by crystal fractionation of garnet. This section has been published in The Journal of Metamorphic Geology (Evans, 2004), and is presented here unchanged. Section C utilises the methods described in the first two sections to determine a metamorphic history for the Garnet Hill and Salmon Hole Brook synclines of central western New Hampshire, USA. The thermal regime of the region during metamorphism was found to be characterised by localised, transient thermal heterogeneities. Two distinct episodes of metasomatism were also defined. Section D utilises the methods described in the first two sections to test a previously defined relative timing scheme for porphyroblast growth that was based on Foliation Intersection Axes preserved within porphyroblast (FIA). Additionally, a tectonic model for central western New Hampshire is presented that explains several key geological features of the region that contradict many of the existing tectonic models.
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Evans, Thomas Philip. "Reconciling the structural and metamorphic record of orogeny in central western New Hampshire through microstructure and garnet isopleth thermobarometry." 2004. http://eprints.jcu.edu.au/1188/1/01front.pdf.

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This thesis consists of four sections, each a stand-alone body of work intended for publication in international journals. The sections are ordered such that they progress in a logical fashion; the first two sections form an introduction to the new analytical techniques developed and utilised within this thesis, the remaining two sections present data and geological interpretations derived from the application of these techniques. Volume 1 contains the text and reference list, whilst Volume 2 contains the figures and appendices. Section A describes the technique of garnet isopleth thermobarometry, and outlines methods for analysing the relative contributions of the sources of error inherent to this technique. Additionally, some insights into the significance of common compositional variations within garnet are provided and discussed. Section B describes a method for calculating the changes in composition of the chemical system from which garnet is growing that are caused by crystal fractionation of garnet. This section has been published in The Journal of Metamorphic Geology (Evans, 2004), and is presented here unchanged. Section C utilises the methods described in the first two sections to determine a metamorphic history for the Garnet Hill and Salmon Hole Brook synclines of central western New Hampshire, USA. The thermal regime of the region during metamorphism was found to be characterised by localised, transient thermal heterogeneities. Two distinct episodes of metasomatism were also defined. Section D utilises the methods described in the first two sections to test a previously defined relative timing scheme for porphyroblast growth that was based on Foliation Intersection Axes preserved within porphyroblast (FIA). Additionally, a tectonic model for central western New Hampshire is presented that explains several key geological features of the region that contradict many of the existing tectonic models.
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Books on the topic "Geology New Hampshire"

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Roadside geology of Vermont and New Hampshire. Missoula: Mountain Press Pub. Co., 1987.

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Hitchcock, Charles H. Description of geological sections crossing New Hampshire and Vermont. [Concord, N.H.?: s.n.], 1987.

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New England Intercollegiate Geological Conference. Meeting. Guidebook for field trips in southwestern New Hampshire, southeastern Vermont, and northcentral Massachusetts: October 14, 15, and 16, 1988, Keene, New Hampshire. Edited by Bothner W. A. Durham, N.H: University of New Hampshire, 1988.

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Degnan, James R. Fracture-correlated lineaments at Great Bay, southeastern New Hampshire. Pembroke, N.H: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Koteff, Carl. Surficial geologic map of the Kingston quadrangle, Rockingham County, New Hampshire. Reston, VA: U.S. Geological Survey, 1994.

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Koteff, Carl. Surficial geologic map of the Townsend quadrangle, Middlesex and Worcester counties, Massachusetts and Hillsborough County, New Hampshire. Reston, VA: U.S. Geological Survey, 1990.

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New England Intercollegiate Geological Conference. Guidebook for field trips in southwestern New Hampshire, southeastern Vermont, and north-central Massachusetts: New England Intercollegiate Geological Conference, 80th annual meeting, October 14, 15 and 16, 1988, Keene, New Hampshire. Edited by Bothner W. A. Durham, NH: Dept. of Earth Sciences, University of New Hampshire, 1988.

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Winegar, Lara. The Old Man of the Mountain. Carmel, California?]: National Geographic School Publishing, Hampton-Brown, 2011.

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Johnson, Carole D. Lithology and fracture characterization from drilling investigations in the Mirror Lake Area, Grafton County, New Hampshire. Pembroke, N.H: U.S. Department of the Interior, U.S. Geological Survey, Toxic Substance Hydrology Program, 1998.

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Johnson, Carole D. Lithology and fracture characterization from drilling investigations in the Mirror Lake area, Grafton County, New Hampshire. Pembroke, N.H: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Book chapters on the topic "Geology New Hampshire"

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Lyons, John B. "Day 5—Geology of central New Hampshire." In A Transect Through the New England Appalachians: Burlington, Vermont to Durham, New Hampshire July 2–8, 1989, 54–58. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft162p0054.

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Bothner, Wallace A. "Day 6—Geology of southeastern and coastal New Hampshire." In A Transect Through the New England Appalachians: Burlington, Vermont to Durham, New Hampshire July 2–8, 1989, 59–64. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft162p0059.

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Iakovleva, Alina I., Florence Quesnel, Christian Dupuis, Jean-Yves Storme, Noémie Breillat, Roberto Magioncalda, Paola Iacumin, et al. "New Integrated High-Resolution Dinoflagellate Cyst Stratigraphy and Litho- and Chemostratigraphy from the Paris and Dieppe–Hampshire Basins for the “Sparnacian”." In Springer Geology, 107–11. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_22.

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Smith, Virginia F. "New Hampshire." In A Scientific Companion to Robert Frost, 67–98. Liverpool University Press, 2018. http://dx.doi.org/10.3828/liverpool/9781942954484.003.0005.

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Frost earned his first of four Pulitzer Prizes for the collection New Hampshire, which was published in 1923. In the years preceding this volume, Frost endured personal heartache, including family deaths and illnesses, as well as increasing professional success. This collection contains many references to geology, astronomy, and exploration, as well as traditional nature themes. The astronomical poems are becoming more theoretical and less observational, incorporating references to new theories about the universe (“Fire and Ice” and “A Never Naught Song.) In a continuation of themes from Mountain Interval, Frost also describes man’s destruction of nature in such poems as “The Census-Taker.” The beauty and challenges of rural life are addressed in poems such as “The Star-Splitter,” “Good-by and Keep Cold,” and “The Need of Being Versed in Country Things.”
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Eby, G. Nelson, Harold W. Krueger, and John W. Creasy. "Geology, geochronology, and geochemistry of the White Mountain batholith, New Hampshire." In Geological Society of America Special Papers, 379–98. Geological Society of America, 1992. http://dx.doi.org/10.1130/spe268-p379.

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Bothner, Wallace A., and Marc C. Loiselle. "Geology of the Belknap Mountains Complex, White Mountain Series, central New Hampshire." In Centennial Field Guide Volume 5: Northeastern Section of the Geological Society of America, 263–68. Geological Society of America, 1987. http://dx.doi.org/10.1130/0-8137-5405-4.263.

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Eusden, J. Dykstra, Mathieu Duvall, and Marita Bryant. "Google Earth mashup of the geology in the Presidential Range, New Hampshire: Linking real and virtual field trips for an introductory geology class." In Google Earth and Virtual Visualizations in Geoscience Education and Research. Geological Society of America, 2012. http://dx.doi.org/10.1130/2012.2492(26).

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Conference papers on the topic "Geology New Hampshire"

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Baker, Sarah W., Jordan Cargill, J. Dykstra Eusden, Dwight C. Bradley, and Richard A. Boisvert. "BEDROCK GEOLOGY OF THE JEFFERSON 7.5’ QUADRANGLE, NEW HAMPSHIRE." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272280.

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Folsom, Liza, J. Eusden, Peter Galloway, and Thomas Sheils. "BEDROCK GEOLOGY, GEOCHRONOLOGY, AND TECTONIC HISTORY OF THE BRONSON HILL BELT IN NORTHERN NEW HAMPSHIRE." In Northeastern Section-56th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021ne-361776.

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Campbell*, Seth, and Steven A. Arcone. "Surficial and bedrock geology mapping with ground-penetrating radar in New England: General results and a case study from Mount Adams, New Hampshire." In SEG Technical Program Expanded Abstracts 2014. Society of Exploration Geophysicists, 2014. http://dx.doi.org/10.1190/segam2014-1636.1.

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Degnan, James R., Stewart F. Clark, and Philip T. Harte. "Integration of Geophysics, Geologic Mapping and Water‐Level Monitoring to Characterize the Hydrogeology of a Fractured Bedrock Site in Berlin, New Hampshire." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2004. Environment and Engineering Geophysical Society, 2004. http://dx.doi.org/10.4133/1.2923391.

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R. Degnan, James, Stewart F. Clark Jr., and Philip T. Harte. "Integration Of Geophysics, Geologic Mapping And Water-Level Monitoring To Characterize The Hydrogeology Of A Fractured Bedrock Site In Berlin, New Hampshire." In 17th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2004. http://dx.doi.org/10.3997/2214-4609-pdb.186.env05.

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Reports on the topic "Geology New Hampshire"

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Ward, Larry, Zachary McAvoy, Maxlimer Coromoto Vallee-Anziani, and Rachel Morrison. Surficial Geology of the Continental Shelf off New Hampshire: Morphologic Features and Surficial Sediment. University of New Hampshire Libraries, 2021. http://dx.doi.org/10.34051/p/2021.31.

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Maps and seismic profiles showing geology of the inner continental shelf, Cape Ann, Massachusetts to New Hampshire. US Geological Survey, 1987. http://dx.doi.org/10.3133/mf1892.

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Bedrock geologic map of Hubbard Brook Experimental Forest and maps of fractures and geology in roadcuts along Interstate 93, Grafton County, New Hampshire. US Geological Survey, 1997. http://dx.doi.org/10.3133/i2562.

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Bedrock geologic map of New Hampshire. US Geological Survey, 1997. http://dx.doi.org/10.3133/70211051.

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Surficial geologic map of the Kingston quadrangle, Rockingham County, New Hampshire. US Geological Survey, 1994. http://dx.doi.org/10.3133/gq1740.

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Surficial geologic map of parts of the Rochester and Somersworth quadrangles, Strafford County, New Hampshire. US Geological Survey, 1991. http://dx.doi.org/10.3133/i2265.

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Simplified geologic map of the Glens Falls 1 degree by 2 degrees Quadrangle, New York, Vermont, and New Hampshire. US Geological Survey, 1990. http://dx.doi.org/10.3133/mf2073.

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Surficial geologic map of the Townsend quadrangle, Middlesex and Worcester Counties, Massachusetts and Hillsborough County, New Hampshire. US Geological Survey, 1990. http://dx.doi.org/10.3133/gq1677.

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Geologic map of the Sherbrooke-Lewiston area, Maine, New Hampshire, and Vermont, United States, and Quebec, Canada. US Geological Survey, 1995. http://dx.doi.org/10.3133/i1898d.

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Isopleth maps showing regional variations in pH of stream water and ground water in relation to geologic setting and known mineral deposits, Glens Falls 1 degree by 2 degrees Quadrangle, New York, Vermont, and New Hampshire. US Geological Survey, 1991. http://dx.doi.org/10.3133/i2161a.

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