Relevant bibliographies by topics / Geology – New York – Dresden

Academic literature on the topic 'Geology – New York – Dresden'

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Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Geology – New York – Dresden"

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Cook, Robert B. "AlmandineNew York City, New York County, New York State." Rocks & Minerals 84, no. 3 (May 2009): 244–52. http://dx.doi.org/10.3200/rmin.84.3.244-252.

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HUTCHINSON, D. R., and JOHN A. GROW. "New York Bight fault." Geological Society of America Bulletin 96, no. 8 (1985): 975. http://dx.doi.org/10.1130/0016-7606(1985)96<975:nybf>2.0.co;2.

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Robinson, Susan. "New York Artist : Darryl Powell." Rocks & Minerals 76, no. 2 (March 2001): 118–19. http://dx.doi.org/10.1080/00357520109603205.

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Robinson, Susan. "Carolyn Graczyk New York Artist." Rocks & Minerals 73, no. 6 (November 1998): 416–17. http://dx.doi.org/10.1080/00357529809603082.

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YOSHITAKE, HIRAKU. "Macrocyrtus imomzodai Barševskis, 2016, a new synonym of Metapocyrtus (Orthocyrtus) orbiferoides Schultze, 1918 (Coleoptera: Curculionidae: Entiminae)." Zootaxa 4254, no. 3 (April 18, 2017): 375. http://dx.doi.org/10.11646/zootaxa.4254.3.5.

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Metapocyrtus (Orthocyrtus) orbiferoides Schultze, 1918 was described based on the female holotype collected from Ilocos Norte, North Luzon, Philippines. Since that time, it has been left unstudied for almost a century until I examined the holotype of M. (O.) orbiferoides in 2010 at Senckenberg Naturhistorische Sammlungen, Museum für Tierkunde, Dresden (SMTD). Recently, Barševskis (2016) described Macrocyrtus imomzodai based on two female specimens from Ilocos Norte, Luzon. Judging from the original description and dorsal and lateral habitus images, it is quite apparent that M. imomzodai is conspecific with M. (O.) orbiferoides. Here I propose a new synonymy based on these examinations. I thank Klaus-Dieter Klass, Olaf Jäger, Christian Schmidt, and Matthias Nuss (SMTD) for their support during my stay in Dresden. My thanks are also due to Steve R. Davis (American Natural History Museum, New York) and Naoko Nakahara (Tsukuba) for their help for preparing the manuscript.
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Barnett, Rosalind C. "Reviews: Women Over Forty: Visions and RealitiesGRAMBSJEAN DRESDEN. New York: Springer Publishing, 1989, 254 pp." Psychology of Women Quarterly 14, no. 4 (December 1990): 618–19. http://dx.doi.org/10.1177/036168439001400401.

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Krinitzsky, Ellis L., and Patrick J. Barosh. "Earthquakes in New York City." Engineering Geology 29, no. 2 (July 1990): 185–89. http://dx.doi.org/10.1016/0013-7952(90)90006-m.

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Chamberlain, Steven C. "A Renaissance in New York Mineralogy." Rocks & Minerals 82, no. 6 (January 2007): 452–57. http://dx.doi.org/10.3200/rmin.82.6.452-457.

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Robinson, George W., and Steven C. Chamberlain. "The Gems of New York State." Rocks & Minerals 82, no. 6 (January 2007): 458–63. http://dx.doi.org/10.3200/rmin.82.6.458-463.

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Lupulescu, Marian. "Minerals from New York State: Pegmatites." Rocks & Minerals 82, no. 6 (January 2007): 494–501. http://dx.doi.org/10.3200/rmin.82.6.494-501.

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Dissertations / Theses on the topic "Geology – New York – Dresden"

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Sirrakos, Georgeos. "Reality pedagogy across contexts : comparing learning environments in the Bronx (New York) and Dresden (Germany)." Thesis, Curtin University, 2012. http://hdl.handle.net/20.500.11937/389.

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The work presented in this thesis was a response to my observations of differences in learning environments and student attitudes toward science between the Bronx, New York and Dresden, Germany when I was a teacher in these locations. In this thesis, I present reality pedagogy as an approach to teaching that allows students from all backgrounds to be successful in science. Reality pedagogy acknowledges the significance of using cultural referents from student experiences as key points from which pedagogy is enacted. Further, reality pedagogy is meant to provide students with classroom agency by including students in the teaching and learning process.This study used a mixed-methods exploratory approach to investigate the outcomes of reality pedagogy in terms of changes in students’ perceptions of the learning environment and their attitudes toward science. The Questionnaire Assessing the Learning Environment and Student Attitudes (QuALESA) was administered to 142 students in grades 8–10 at Bronx High School in New York City and the International School of Dresden in Dresden, Germany. The QuALESA was created by combining learning environment scales from the Constructivist Learning Environment Survey (CLES) and the What Is Happening In this Class? (WIHIC) questionnaire with attitude scales from the Test of Science-Related Attitudes (TOSRA). In addition, qualitative data were collected from cogenerative dialogues, classroom observations, and semi-structured student interviews and were used to support findings from the QuALESA.Because one of the aims of the study was to establish the validity and reliability of the QuALESA, it was administered at the beginning and conclusion of the 2010–2011 academic year in two high school science classrooms in the Bronx and five high school science classrooms in Dresden. Data analyses supported the factorial validity and reliability of the QuALESA for use with these samples.Overall changes in student perceptions of the learning environment and attitudes toward science in response to reality pedagogy were also investigated. MANOVA revealed significant improvements between pretest and posttest for six of the seven scales (Involvement, Cooperation, Personal Relevance, Critical Voice, Shared Control, and Enjoyment of Science Lessons). Classroom observations supported the changes revealed by the quantitative data analyses and showed shifts in teaching practices aimed at more involvement of students in the teaching and learning of science. However, when differences between how reality pedagogy manifested itself in classroom in the Bronx and Dresden were also explored in terms of student learning environment perceptions and attitudes toward science, it was found that students in Dresden had significantly higher pretest scores for six scales on the QuALESA. However, these pretest differences between the two locations were no longer present by the time of the posttest.While the quantitative data indicated that, over time, the perceptions and attitudes of students from the Bronx became more closely aligned with those of students from Dresden, the qualitative data revealed differences in how reality pedagogy was enacted in each geographic area. Students in the Bronx focused more on changing teacher practices to engage students more in science, whereas students in Dresden were more concerned with increasing their roles as co-teachers and sharing control with the teacher.Finally, when the quantitative data were analyzed to explore associations between students’ perceptions of their learning environment and their attitudes toward science, positive and statistically significant associations emerged between several learning environment scales and the attitude scales.Overall, the findings of this study add to the body of evidence concerning the effectiveness of employing reality pedagogy as a pedagogical approach to teach science across a variety of contexts.
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Weremeichik, Jeremy M. "Paleoenvironmental reconstruction by identification of glacial cave deposits, Helderberg Plateau, Schoharie County, New York." Thesis, Mississippi State University, 2013. http://pqdtopen.proquest.com/#viewpdf?dispub=1536097.

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Eight dissolution caves from the Helderberg Plateau in Schoharie County, New York were studied to investigate unusual sediment packages previously interpreted to be deposits laid down during stagnant ice-cover conditions of the Wisconsin glaciation. The sediment package, consisting of white finely laminated silts and clays are overlain by coarse gravels, in turn overlain by dark silts and clays. Analysis of 63 sediment samples was inconclusive in terms of organic content, but indicated a higher degree of fine-grained calcite material in the white clays than in the overlying units. The caves with the white clays exist only within the footprint of Glacial Lake Schoharie, with lower elevation caves containing a thicker white clay sequence, a measure of the duration of lake cover. The sediment sequence represents glacial rock flour formed under stagnant lake conditions, overlain by outwash deposits emplaced during lake termination, and more recent sediment from soil-loss deposition.

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Cooper, Max. "Verification of post-glacial Speleogenesis and the origins of Epigene Maze Caves in New York." Thesis, Mississippi State University, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1554909.

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Dissolutional features called karst exist on the surface, and in the subsurface as caves. In glaciated regions caves were thought to be post-glacial in origin. Work in the 1970s demonstrated that pre-glacial caves existed, but did not answer if a cave could form post-glacially. A model proposed by Mylroie and Carew (1987) states that a post-glacial cave would be controlled entirely by glacial features and the deranged drainage of glaciated terrains. Caves known as maze caves form at maximum rates, and could form to navigable size in the time since deglaciation. Maze caves form in the shallow subsurface, allowing them to be removed in subsequent glaciations. GIS water flow analysis, and calculation of formation times using cross-section data demonstrates that maze caves in the glaciated region of New York are post-glacial in origin fitting in the deranged drainage and forming in the time since deglaciation.

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Smith, Jason J. "A reinterpretation of the sedimentology and stratigraphy of the upper Silurian-lower Devonian Manlius Formation in upstate New York." Diss., Online access via UMI:, 2009.

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Sessa, Jocelyn A. "The dynamics of rapid, asynchronous biotic turnover in the middle Devonian Appalachian basin of New York : a thesis /." Connect to The dynamics of rapid, asynchronous biotic turnover in the middle Devonian Appalachian basin of New York (Online), 2003. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=1054576413.

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Yakovlev, Petr V. "Transitions in Structural Styles and Trends within the Northern Appalachian Hudson Valley Fold-Thrust Belt Near Catskill, New York." Thesis, Boston College, 2010. http://hdl.handle.net/2345/1191.

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Thesis advisor: Yvette D. Kuiper
The Hudson Valley fold-thrust belt (HVB) is a narrow belt of deformed Upper Ordovician to Middle Devonian clastic and carbonate strata exposed in the western Hudson Valley of New York State. Geologic mapping at a scale of 1:10,000 was carried out near the town of Catskill. The southern portion of the map area includes a large doubly-plunging structure which features a fault-dominated southern portion plunging towards 017° and a northern fold-dominated, 206° trending, southerly plunging segment. A relay structure between two major faults or fault systems is interpreted as existing between the two domains. Farther north, the HVB narrows and folds plunge shallowly towards 212°, and then widens with folds plunging shallowly towards 017°. The changes can be explained by a localized increase in slip on the Austin Glen Detachment in the center of the map area, and subsequent loss of slip towards the north
Thesis (BA) — Boston College, 2010
Submitted to: Boston College. College of Arts and Sciences
Discipline: College Honors Program
Discipline: Geology and Geophysics
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BARTHOLOMEW, ALEXANDER. "CORRELATION OF HIGH ORDER CYCLES IN THE MARINE-PARALIC TRANSITION OF THE UPPER MIDDLE DEVONIAN (GIVETIAN) MOSCOW FORMATION, EASTERN NEW YORK STATE." University of Cincinnati / OhioLINK, 2002. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1022593337.

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Brink, Ryan A. "Sedimentologic Comparison Of The Late/lower Early Middle Cambrian Altona Formation And The Lower Cambrian Monkton Formation." ScholarWorks @ UVM, 2015. http://scholarworks.uvm.edu/graddis/370.

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The Altona Formation represents the oldest Cambrian sedimentary unit in northern New York, recording cyclic deposition in shallow marine and fluvial environments under both fair-weather and storm conditions. Five outcrops and one well log were measured and described at the centimeter scale and the top and bottom contacts of the Altona were identified. Based on the recognition of sedimentary structures such as hummocky cross stratification, oscillatory ripples, graded bedding, trough and tabular cross stratification, and bioturbation, as well as subtle lithologic changes, six lithofacies representing non-marine, middle to upper shoreface, offshore, and carbonate ramp environments were identified. The top contact with the overlying Ausable Formation is characterized by inter-tonguing marine to non-marine siltstones and cross stratified medium sandstones. The lowermost Altona is found to lie only one meter above Precambrian basement and is interpreted to be the only non-marine facies in this unit. Throughout the 84-meter thick section, stratigraphy records a transition from upper/middle shoreface to carbonate ramp deposition and offshore muds before cycling between upper shoreface, carbonate ramp and non-marine deposits. Based on parasequence architecture, this section of rock is interpreted to represent the transition from the transgressive systems tract to the highstand systems tract. Thin sections analysis from each lithofacies quantified grain size and composition and identified a provenance. Modal analysis data from clastic lithofacies reveals subarkose to arkose sandstones with an accessory mineral suite including ilmenite, apatite, rutile, and zircon. Integrating the compositional data, particularly the accessory mineral suite, with detrital zircon dates of 1000 - 1300 Ma (Chiarenzelli et al., 2010) suggests that the Grenville Adirondacks in particular the AMCG suit and Lyon Mountain Granite are a likely source rock. Comparison with the Monkton Formations of Vermont suggest that these two units were deposited under similar sea level conditions and are therefore correlative. Provenance study suggests that they were both sourced form the Adirondack Mountains. The major difference is in their depositional environments as the Monkton represents deposition of predominantly tidally influenced deltaic environment. The environmental processes acting on the two units suggests that the paleogeography of the Iapetus margin in this area was an embayed coastline.
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Cornell, Sean Richard. "Sequence Stratigraphy and Event Correlations of Upper Black River and Lower Trenton Group Carbonates of Northern New York State and Southern Ontario, Canada." University of Cincinnati / OhioLINK, 2001. http://rave.ohiolink.edu/etdc/view?acc_num=ucin997444936.

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Smidt, Samuel J. "A comparison of hyporheic transport at a constructed stream restoration structure and natural riffle feature, West Branch Owego Creek, New York, USA." Thesis, University of Iowa, 2014. https://ir.uiowa.edu/etd/3192.

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While restoring hyporheic flowpaths has been cited as a benefit to stream restoration structures, little documentation exists confirming that constructed restoration structures induce hyporheic exchange comparable to natural stream features. This study compares a stream restoration structure (cross-vane) to a natural feature (riffle) concurrently in the same stream reach using time-lapsed electrical resistivity (ER) tomography. Using this hydrogeophysical approach, I am able to quantify hyporheic extent and transport beneath the cross-vane structure and riffle. I interpret from the geophysical data that the cross-vane and natural riffle induced spatially and temporally unique hyporheic extent and transport, and the cross-vane created both spatially larger and temporally longer hyporheic flowpaths than the natural riffle. Tracer from the 4.67-hr injection was detected along flowpaths for 4.6-hrs at the cross-vane and 4.2-hrs at the riffle. The spatial extent of the hyporheic zone at the cross-vane was 12% larger than at the riffle. I compare ER results of this study to vertical fluxes calculated from temperature profiles and conclude significant differences in the interpretation of hyporheic transport from these different field techniques. Results of this study demonstrate a high degree of heterogeneity in transport metrics at both the cross-vane and riffle and significant differences between the hyporheic flowpath networks at the two different features. Our results suggest that restoration structures may be capable of creating sufficient exchange flux and residence times to achieve the same ecological functions as natural features, but engineering of the physical and biogeochemical environment may be necessary to realize those benefits.
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Books on the topic "Geology – New York – Dresden"

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Sougioutzoglou-Seraidarē, Nelly's. Nelly: Dresden, Athens, New York. Munich: Prestel, 2001.

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VanDiver, Bradford B. Roadside geology of New York. Missoula: Mountain Press Pub. Co., 1994.

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Roadside geology of New York. Missoula: Mountain Press Pub. Co., 1985.

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J, Kloc Gerald, Brett Carlton E, and Paleontological Research Institution (Ithaca, N.Y.), eds. Trilobites of New York: An illustrated guide. Ithaca [N.Y.]: Comstock Pub. Associates, 2002.

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Baskerville, Charles A., Nocholas K. Coch, Sidney Horenstein, Martin Prinz, John H. Puffer, Geneva R. Roberts-Dolgin, and Dennis Weiss, eds. Geology and Engineering Geology of the New York Metropolitan Area. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft361.

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1920-, Isachsen Yngvar W., ed. Geology of New York: A simplified account. Albany, NY: New York State Museum, 1991.

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W, Fisher Donald. Bedrock geology of the Glens Falls-Whitehall region, New York. Albany: University of the State of New York, the State Education Department, 1985.

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Ratcliffe, Nicholas M. Bedrock geology and seismotectonics of the Oscawana Lake Quadrangle, New York. [Washington]: U.S. G.P.O., 1992.

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Dresden, Tuesday, February 13, 1945. New York: HarperCollins, 2004.

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Dresden, Tuesday, February 13, 1945. New York: HarperCollins, 2005.

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Book chapters on the topic "Geology – New York – Dresden"

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Horenstein, Sydney. "Building stones of the New York City area." In Geology and Engineering Geology of the New York Metropolitan Area, 2–14. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft361p0002.

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Puffer, John H. "Geology of northeastern New Jersey." In Geology and Engineering Geology of the New York Metropolitan Area, 26–38. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft361p0026.

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Grasso, Thomas X. "Amos Eaton and early New York State geology." In Boston to Buffalo, in the Footsteps of Amos Eaton and Edward Hitchcock: Boston, Massachusetts to Washington, D.C. June 28–July 8, 1989, 43–48. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft169p0043.

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Baskerville, Charles A. "Introduction." In Geology and Engineering Geology of the New York Metropolitan Area, 1. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft361p0001.

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Coch, Nicholas K., and Dennis Weiss. "Environmental geology and geological development of the lower Hudson estuary and New York Harbor." In Geology and Engineering Geology of the New York Metropolitan Area, 15–25. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft361p0015.

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Baskerville, Charles A. "New York City: Juxtaposition of Cambrian and Ordovician miogeoclinal and eugeoclinal rocks." In Geology and Engineering Geology of the New York Metropolitan Area, 39–48. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft361p0039.

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Prinz, Martin. "The American Museum of Natural History." In Geology and Engineering Geology of the New York Metropolitan Area, 49–50. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft361p0049.

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Roberts-Dolgin, Geneva R. "The geology of Staten Island and western Long Island, Kings and Queens counties, New York." In Geology and Engineering Geology of the New York Metropolitan Area, 51–59. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft361p0051.

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Baskerville, Charles A., and Robert H. Fakundiny. "Engineering Geology of New York City: Continuing Value of Geologic Data." In Earth Science in the City: A Reader, 43–59. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/sp056p0043.

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Marshak, Stephen. "Introduction to Applachian geology: A geologicl sketch of southeastern New York State." In Structures of the Appalachian Foreland Fold-Thrust Belt: New York City, to Knoxville, Tennessee, June 27–July 8, 1989, 3–6. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft166p0003.

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Conference papers on the topic "Geology – New York – Dresden"

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Kelly, William M., Jean Neubeck, David A. Franzi, Jane Blair, and April Friedman. "PREPARING FOR GEOLOGY LICENSURE IN NEW YORK - A PROGRESS REPORT." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272358.

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Dineen, Robert J. "GLACIAL GEOLOGY OF THE ALBANY 15-MINUTE QUADRANGLE, EASTERN NEW YORK STATE." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272021.

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Schimmrich, Steven H. "A GEOLOGY FIELD COURSE INCORPORATING THE HISTORY OF THE HUDSON VALLEY REGION OF NEW YORK." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-309923.

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Gocklin, Christopher R., Harry Maisch, Martin A. Becker, John A. Chamberlain, Michael Dubaldi, Alexander Bartholomew, and Rebecca B. Chamberlain. "RECONSTRUCTING SURFICIAL GEOLOGY IN THE NORTHERN NEW JERSEY PIEDMONT UTILIZING FOSSILIFEROUS GLACIAL ERRATICS FROM THE LOWER AND MIDDLE DEVONIAN OF EASTERN NEW YORK." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-289906.

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Heyer, Mark, and David A. Franzi. "REASSESSING THE SURFICIAL GEOLOGY AND DEGLACIAL CHRONOLOGY OF THE LOWER SARANAC VALLEY, NORTHEASTERN NEW YORK USING HIGH-RESOLUTION LIDAR ELEVATION AND HILLSHADE MODELS." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328504.

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Jordan, Eric. "THE GEOLOGICAL FINDINGS OF THE NYCDEP BYPASS TUNNEL ALIGNMENT AND IMPLICATIONS ON THE STRUCTURAL GEOLOGY OF THE MID-HUDSON VALLEY OF NEW YORK." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-382557.

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Schütte, Jörg, and Sven Scholz. "Recent Experience on Guideway Intrusion Detection System Implementations." In 2017 Joint Rail Conference. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/jrc2017-2334.

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During the last decade, several Public Transportation Operators have started to test and implement technical equipment that shall detect passengers or objects intruding the clearance profile of trains in the station area. The deployed or tested systems typically supervise the track area of subways or light rails and shall stop incoming trains if an obstacle has been detected on the tracks (Guideway Intrusion Detection System, GIDS). While some scientific and operational publications can be found in the literature for Onboard Obstacle Detection Systems and on different technical solutions for Guideway Intrusion in general, there are virtually none on planning and operations experience for Wayside GIDS in transit applications. The paper therefore reports on the basic intention and operation of (wayside) GIDS in Unmanned and Driver Operations and findings about detection efficiency and feasibility. Some critical issues had been observed in most implementations and will be discussed in this overview paper. TelSys GmbH has been working with researchers from TU Dresden on Video GIDS Technology in multiple installations, accumulated substantial statistics of GIDS behavior in diverse field demonstrators (Prague, Berlin, New York City, Munich) and assessed the operational results of GIDS technologies over the years. The Video GIDS is therefore introduced as an illustration example, while the considered aspects are applicable to all GIDS Technologies.
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Reports on the topic "Geology – New York – Dresden"

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Bélanger, J. R., A. Moore, and A. Prégent. Surficial geology, digital map, Morrisburg, Ontario-New York (31B/14). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/209121.

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Lewis, C. F. M., B. J. Todd, and G. D. M. Cameron. Seismostratigraphy of western Lake Ontario, Ontario and New York: Quaternary geology and implications for groundwater discharge. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/299669.

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Bedrock geology and seismotectonics of the Oscawana Lake Quadrangle, New York. US Geological Survey, 1992. http://dx.doi.org/10.3133/b1941.

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Geology of the Birch Creek area, St. Lawrence County, New York. US Geological Survey, 1988. http://dx.doi.org/10.3133/i1645.

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Geology, hydrology, and ground-water flow near the Akron municipal well, Erie County, New York. US Geological Survey, 1996. http://dx.doi.org/10.3133/wri964193.

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Generalized stratigraphy, surficial geology, types of aquifers, and 1988-89 ground-water pumpage in eastern Saratoga County, New York. US Geological Survey, 1994. http://dx.doi.org/10.3133/wri934029.

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Surficial geology and ground-water availability in the Allegheny River Basin and part of the Lake Erie Basin, New York. US Geological Survey, 1986. http://dx.doi.org/10.3133/wri864041.

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Geology and hydrology of the Onondaga aquifer in eastern Erie County, New York; with emphasis on ground-water-level declines since 1982. US Geological Survey, 1987. http://dx.doi.org/10.3133/wri864317.

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9

Glacial geology and the origin and distribution of aquifers at the Valley Heads moraine in the Virgil Creek and Dryden Lake-Harford Valleys, Tompkins and Cortland counties, New York. US Geological Survey, 1993. http://dx.doi.org/10.3133/wri904168.

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