Mapping, Petrological and Geochemical Explorations of the Massabesic Gneiss Complex in New Hampshire Charles M
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The Geology of the Saddleback Mountain Area, Northwood Quadrangle, Southeastern New Hampshire
University of New Hampshire University of New Hampshire Scholars' Repository New England Intercollegiate Geological NEIGC Trips Excursion Collection 1-1-1984 The geology of the Saddleback Mountain Area, Northwood quadrangle, southeastern New Hampshire Whitaker, Laura R. Follow this and additional works at: https://scholars.unh.edu/neigc_trips Recommended Citation Whitaker, Laura R., "The geology of the Saddleback Mountain Area, Northwood quadrangle, southeastern New Hampshire" (1984). NEIGC Trips. 352. https://scholars.unh.edu/neigc_trips/352 This Text is brought to you for free and open access by the New England Intercollegiate Geological Excursion Collection at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in NEIGC Trips by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. B6-1 207 THE GEOLOGY OF THE SADDLEBACK MOUNTAIN AREA, NORTHWOOD QUADRANGLE, SOUTHEASTERN NEW HAMPSHIRE Laura R. Whitaker Department of Geology The College of Charleston Charleston. SC 2942^ Introduction Saddleback Mountain is a four-peaked saddle-shapped mountain located 39 km west of Portsmouth, NH (Figure 1). The mountain lies along the boundary between the New England Uplands and the Seaboard Lowlands Sections of the New England Physiographic Province of Fenneman (1938). It also lies adjacent to the western boundary of the Massabesic Gneiss Complex as designated by Anderson (1978). Figure 2 of this text is a generalized Geologic Map of Southeastern New Hampshire compiled from Billings (1956) and later workers cited in the references from Figure 1. Portions of Figure 2 show that the Saddleback Mountain area is on strike with two convergent fault zones which are postulated to be of regional tectonic significance: the Nurambego of southern Maine (Hussey and Pankiwskyj, 1976; Hussey and Newberg, 1978), and the Pinnacle-Campbell-Hill-Hall Mountain Faults mapped by Camein (1976). -
Town of Auburn, New Hampshire Hazard Mitigation Plan Executive Summary
TOWN OF AUBURN, NEW HAMPSHIRE Town of Auburn, New Hampshire, Town Offices HAZARD MITIGATION PLAN 2018 TOWN OF AUBURN NEW HAMPSHIRE HAZARD MITIGATION PLAN October 2018 Prepared for the Town of Auburn, NH, NH Homeland Security & Emergency Management (NHHSEM) and Federal Emergency Management Agency (FEMA) by The Southern New Hampshire Planning Commission with assistance from the Auburn Hazard Mitigation Committee October, 2018 October 22, 2018 Public Hearing Date October 22, 2018 Adoption Date Final Plan Acknowledgements Southern NH Planning Commission and the Town of Auburn wish to thank the following individuals for serving on the Town’s Hazard Mitigation Committee and for their assistance in the development of this Plan: Acknowledgements Appreciation is extended to the following people for contributing their time and effort to complete the Auburn Hazard Mitigation Plan: 2016-2018 Auburn Hazard Mitigation Committee Members Edward Gannon Fire Chief/Emergency Director, Town of Auburn, Chair Lori Collins Principal, Auburn Village School Lillian Deeb Police, Town of Auburn Mike Dross Road Agent, Town of Auburn Bill Herman Town Administrator, Town of Auburn Ray Pelton Police Chief, Town of Auburn Carrie Rouleau-Cote Building Inspector, Town of Auburn Denise Royce Planning/Land Use Administrator, Town of Auburn Jim Scalnier Fire Inspector, Town of Auburn Madeline DiIonno Southern New Hampshire Planning Commission Cameron Prolman Southern New Hampshire Planning Commission Derek Shooster Southern New Hampshire Planning Commission Zachary Swick -
Gold in New Hampshire
GEO-1 2020 Gold in New Hampshire Yes! New Hampshire has gold! However, to date, only small quantities have been found in some of the state’s bedrock (the solid rock under the soil) and in the gravels at the bottom of some streams (as placer deposits). When gold is found in the bedrock, it usually occurs in veins – long, narrow mineral rich “streaks.” It is removed by breaking up the rock and extracting the gold. New Hampshire has a brief but colorful history of hard rock mining. Gold was discovered in Lyman, N.H., in 1864, sparking a minor rush. Several small mines soon opened in the Bath, N.H., area. These small mines supported two milling operations. About $50,000 worth of gold (at period value) was shipped to the Philadelphia National Mint before economic circumstances closed operations in 1878. A much smaller amount of gold was also shipped to the mint from the Diamond Ledge Mine in Ossipee. None of these mines operated for very long. Occurrence Gold is found in certain types of rocks, formed by geologic processes. The weathering of New Hampshire’s gold bearing bedrock broke the rock apart naturally. However, gold does not weather, and this allowed the more resistant flakes and nuggets of gold to be washed away by running water. Gold is approximately 19 times heavier than the same volume of water and gets left on the stream bottom with other heavy rock and mineral fragments. Gold found in stream gravel is known as a placer deposit. Panning and dredging are methods of separating the heavy gold flakes and nuggets from the stream gravels. -
Bedrock Geologic Map of the Nashua South Quadrangle, Hillsborough County, New Hampshire, and Middlesex County, Massachusetts
Prepared in cooperation with the Commonwealth of Massachusetts, Massachusetts Geological Survey and the State of New Hampshire, New Hampshire Geological Survey Bedrock Geologic Map of the Nashua South Quadrangle, Hillsborough County, New Hampshire, and Middlesex County, Massachusetts By Gregory J. Walsh, Richard H. Jahns, and John N. Aleinikoff Pamphlet to accompany Scientific Investigations Map 3200 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2013 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Walsh, G.J., Jahns, R.H., and Aleinikoff, J.N., 2013, Bedrock geologic map of the Nashua South quadrangle, Hillsbor- ough County, New Hampshire, and Middlesex County, Massachusetts: U.S. Geological Survey Scientific Investigations -
Deglaciation of the Northwestern White Mountains, New Hampshire
Géographie physique et Quaternaire, 1999, vol. 53, n° 1, p. 59-77, 14 fig., 3 tabl. DEGLACIATION OF THE NORTHWESTERN WHITE MOUNTAINS, NEW HAMPSHIRE Woodrow B. THOMPSON*, Brian K. FOWLER** and Christopher C. DORION***, respectively Maine Geological Survey, 22 State House Station, Augusta, Maine 04333-0022 U.S.A.; Mount. Washington Observatory, P. O. Box 2310, North Conway, New Hampshire 03860 U.S.A. and Geological Services, 79 Bennoch Rd., Orono, Maine 04473 U.S.A. , 1999, vol. 53, n° 1, 14 fig., 3 tabl., 53(1), 1999W. B. THOMPSON, B. K. FOWLER and C. C. DORION ABSTRACT The mode of deglaciation in the RÉSUMÉ La déglaciation du nord-ouest des ZUSAMMENFASSUNG Enteisung der nord- northwestern White Mountains of New Hamp- White Mountains, au New Hampshire (E.- westlichen White Mountains, New Hampshire. shire has been controversial since the mid U.A.). Le mode de déglaciation du nord-ouest Die Art des Abschmelzens in den nordwestli- 1800’s. Early workers believed that active ice des White Mountains a fait l’objet de contro- chen White Mountains von New Hampshire ist deposited the Bethlehem Moraine complex in verses depuis le milieu du XIXe siècle. Les pre- seit Mitte des 19. Jahrhunderts umstritten ge- the Ammonoosuc River basin during reces- miers chercheurs ont supposé que le wesen. Die ersten Forscher glaubten, dass ak- sion of the last ice sheet. In the 1930’s this de- complexe morainique de Bethlehem dans le tives Eis die Bethlehem-Moräne-Einheit glaciation model was replaced by the concept bassin de l’Ammonoosuc River avait été mis während des Rückzugs der letzten Eisdecke im of widespread simultaneous stagnation and en place par la glace active au cours du recul Becken des Ammonoosuc-Flusses ablagerte. -
Stratigraphy and Ductile Structure of the Presidential Range, New Hampshire: Tectonic Implications for the Acadian Orogeny
Stratigraphy and ductile structure of the Presidential Range, New Hampshire: Tectonic implications for the Acadian orogeny J. Dykstra Eusden Jr. John M. Garesche Aaron H. Johnson Jenna-Marie Maconochie Department of Geology, Bates College, Lewiston, Maine 04240 Steven P. Peters Jonathan B. O’Brien Beth L. Widmann } ABSTRACT mation is interpreted as an olistostromal fected by the Early Devonian Acadian melange and has been subdivided into three orogeny. These rocks are extremely well ex- The Presidential Range of New Hamp- different members and six submembers on posed, thus offering a rare opportunity to shire with its unique high relief contains ex- the basis of lithologic variations in the accurately and clearly describe the complex ceptionally well exposed rocks of the Aca- gneiss and subordinate units. stratigraphic and structural features in this dian orogenic hinterland. These rocks are The Presidential Range preserves three part of the northern Appalachians. Though within the Central Maine terrane, a belt of phases of ductile folding (F1, F2, and F3) the Acadian orogeny has been comprehen- complexly metamorphosed and deformed and a single phase of thrust faulting (T1). sively studied by numerous geologists, Aca- Silurian and Devonian metasedimentary Well-constrained southeast-, east- or north- dian tectonic models remain controversial rocks. The Presidential Range lies between east-facing directions and consistent asym- due to the lack of distinctive lithotectonic regions to the south dominated by refolded metry of F1 nappe limbs suggest that nappe assemblages. Notably absent from the nappes and synkinematic high-grade re- vergence was easterly. Severe refolding of Acadian orogen is obducted ocean crust, gional metamorphism and regions to the some nappes resulted during F2 collapse accretionary melange, or unequivocal arc northeast dominated by overlapping multi- of the nappe pile. -
Surficial Geology of the Merrimack River Valley Between Manchester and Nashua, New Hampshire
University of New Hampshire University of New Hampshire Scholars' Repository New England Intercollegiate Geological NEIGC Trips Excursion Collection 1-1-1971 Surficial Geology of the Merrimack River Valley Between Manchester and Nashua, New Hampshire Koteff, Carl Stone, Byron D. Follow this and additional works at: https://scholars.unh.edu/neigc_trips Recommended Citation Koteff, Carl and Stone, Byron D., "Surficial Geology of the Merrimack River Valley Between Manchester and Nashua, New Hampshire" (1971). NEIGC Trips. 156. https://scholars.unh.edu/neigc_trips/156 This Text is brought to you for free and open access by the New England Intercollegiate Geological Excursion Collection at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in NEIGC Trips by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. 100 TRIP B-4 SURFICIAL GEOLOGY OF THE MERRIMACK RIVER VALLEY BETWEEN MANCHESTER AND NASHUA, NEW HAMPSHIRE Carl Koteff and Byron D. Stone_/ U.S. Geological Survey Boston, Massachusetts This trip will examine evidence for two tills thought to represent separate glaciations, and evidence for a minor readvance during the last glaciation. Other stops include exposures related to glacial Lake Merrimack, postlake erosion, and late glacial eolian activity. REFERENCES CITED: Goldthwait, J. W., Goldthwait, Lawrence, and Goldthwait, R. P., 1951, The geology of New Hampshire, Part I, Surficial geology: Concord, N. H., New Hampshire State Plan, and Devel. Comm., 83 p. Koteff, Carl, 1970, Surficial geologic map of the Milford quadrangle, Hillsborough Country, New Hampshire: U.S. Geol Survey, Geol. Quad. Map GQ-881. -
Surficial Geology Map of the Jefferson 7.5' Quadrangle, New Hampshire
Surficial Geology of the Jefferson 7.5' Quadrangle, New Hampshire 71°30'0"W 71°27'30"W 71°25'0"W 71°22'30"W 44°30'0"N 44°30'0"N 32 td td td 180 td Pt DESCRIPTION OF MAP UNITS Ha Pg 220 Pt Stream or lake 36 Artificial fill— Earth m ate rial of various sorts, use d as road fill. Shown af Pt 110 7 only whe re thick e nough to alte r the top ograp hic m ap contours. 50 td Qls HOLOCEN E DEP OSITS 122 Stream alluvium— Sand , grave l, and silt d e p osite d on the flood p lains of Qf Ha Pg Qf td stre am s. Unit m ay includ e som e we tland are as. 24 Wetland deposits— P e at, m uck, silt, and clay. De p osite d in p oorly d raine d 20 Hw 3 8 Qfb1 are as. 6 6 Qfb1 120 QUATERN ARY DEP OSITS td 3 22 131 Qfb2 Israel Valley deposits — Unclassifie d glacial to p ostglacial sand and Qirvd grave l in the Israe l Rive r valle y. Most of this unit occurs in the ad jace nt Mount Dartm outh q uad rangle to the south (Fowle r and Barke r, 2015). Qfb1 td Stream terraces — Sand and grave l d e p osite d on form e r flood -p lain td Qst Pg surface s along the Israe l Rive r and othe r stre am s. Qfg Fan deposits (undifferentiated) — Alluvial fans form e d along the m id to Qf Pt Qls lowe r re ache s of stre am s that d rain the ste e p m ountain slop e s which occur ove r m uch of the m ap are a. -
Guidebook for Field Trips in Central New Hampshire and Contiguous Areas
DISCLAIMER Before visiting any of the sites described in the New England Intercollegiate Geological Conference guidebooks, you must obtain permission from the current landowners. Landowners only granted permission to visit these sites to the organizers of the original trips for the designated dates of the conference. It is your responsibility to obtain permission for your visit. Be aware that this permission may not be granted. Especially when using older guidebooks in this collection, note that locations may have changed drastically. Likewise, geological interpretations may differ from current understandings. Please respect any trip stops designated as “no hammers”, “no collecting” or the like. Consider possible hazards and use appropriate caution and safety equipment. NEIGC and the hosts of these online guidebooks are not responsible for the use or misuse of the guidebooks. ilnL(jszutu of JLiiPiaxij Ell, 3 4bOO 0Q^7^ 3D3M NEW ENGLAND INTERCOLLEGIATE GEOLOGICAL CONFERENCE GUIDEBOOK for field trips in Central New Hampshire and Contiguous Areas John B. Lyons Glenn W. Stewart Editors 63rd Annual Meeting October 2 and 3, 1971 Concord, New Hampshire o > Conference Organization Herbert Tischler Glenn W. Stewart John B. Lyons Dabney M. Caldwell, Secretary, New England Intercollegiate Geological Conference Field Trip Leaders Franz E. Anderson, University of New Hampshire, Durham, N.H. Wallace A. Bothner , University of New Hampshire, Durham, N.H. Russell G. Clark, Dartmouth College, Hanover, N.H. Evan Englund, Dartmouth College, Hanover, N. H. Henri E. Gaudette, University of New Hampshire, Durham, N.H. Richard P. Goldthwait, Ohio State University, Columbus, Ohio Robert C. Greene, U.S. Geological Survey, Menlo Park, Calif. -
The Nappe Theory in the Connecticut
American Mineralogist, Volume 76, pages 689-712, 1991 The nappetheory in the ConnecticutValley region: Thirty-five years since Jim Thompson'sfirst proposal Pprn,nRonrNsor.l Department of Geology and Geography,University of Massachusetts,Amherst, Massachusetts01003, U.S.A. Prrnn J. TnonrpsoN Department of Geology, Cornell College,Mount Vernon, Iowa 52314, U.S.A. D,q,vroC. Er-nnnr Department of Geology, Middlebury College,Middlebury, Vermont 05753, U.S.A. AssrRAcr The nappe theory in the Bronson Hill anticlinorium of the Connecticut Valley region began with Jim Thompson's analysis of the structure of SkitchewaugMountain in 1954. By 1968 the theory included the recognition of three giant fold nappesformed early in the Devonian Acadian orogeny, with tens of kilometers of east to west overfolding. These were, from lowest to highest,the Cornish, the Skitchewaug,and the Fall Mountain nappes. Recognition ofthe nappeswas basedon careful tracing ofa previously recognizedsequence of distinctive Ordovician, Silurian, and Lower Devonian stratigraphic units that were metamorphosed to the chlorite zone through sillimanite-orthoclase zone. Some of these units proved to be fossiliferous even in the sillimanite zone. Early on, a relationship was recognizedbetween high metamorphic grade and high structural level, implying overfold- ing ofhotter rocks onto cooler ones. In the 1970sdetailed remapping suggestedthat the system included not three but four fold nappes. Some of the rocks previously assignedto the Skitchewauglevel proved to belong to the Bernardston nappe beneath the Skitchewaug.Although shearedand atten- uated fold limbs were part of the nappe theory before 1980, it was only after this that major thrust faults were considered to be important. -
Weare Hazard Mitigation Plan 2018
TOWN OF WEARE, NEW HAMPSHIRE River Road Bridge over the Piscataquog River, replaced in 2016 HAZARD MITIGATION PLAN UPDATE 2018 TOWN OF WEARE NEW HAMPSHIRE HAZARD MITIGATION PLAN UPDATE Adopted November 5, 2018 Prepared by the Southern New Hampshire Planning Commission The preparation of this document has been financed in part by a grant from the State of New Hampshire Department of Safety, Division of Homeland Security and Emergency Management. Acknowledgements Appreciation is extended to the following people for contributing their time and effort to complete the Weare Hazard Mitigation Plan Update 2018: Weare Hazard Mitigation Committee Members Sean Kelly - Chief of Police, Weare Police Department Naomi Bolton - Town Administrator Sue Tuthill - Administrative Secretary, Weare Fire Department Robert Vezina - Emergency Management Director & Fire Chief, Town of Weare Benjamin Knapp - Director, Weare Department of Public Works Chip Meany - Land Use Coordinator, Weare Building Department Tom Clow - Weare Board of Selectmen Chip Meany - Building Inspector Marjory Burke - School Board Representative Aprylle Desrosiers - Associate Principal, John Stark Regional High School Emily Dauphinais - Administrative Secretary, Police Department Thanks also to: • The New Hampshire Department of Safety, Homeland Security and Emergency Management,, which developed the State of New Hampshire Multi-Hazard Mitigation Plan Update 2013; • The Southwest Region Planning Commission, which developed Hazard Mitigation Planning for New Hampshire Communities; and • The Auburn, Bedford, Chester, Derry, Goffstown, Hooksett, Londonderry, Manchester, and New Boston Hazard Mitigation Committees and their respective Hazard Mitigation Plans. All the above publications served as models for this plan. "We will of course be there to help after disaster strikes, but as you all know, there’s no substitute for mitigation before it does... -
Graphite Vein Deposits of New Hampshire
University of New Hampshire University of New Hampshire Scholars' Repository New England Intercollegiate Geological NEIGC Trips Excursion Conference Collection 1-1-1988 Graphite Vein Deposits of New Hampshire Rumble, D. Chamberlain, C.P. Follow this and additional works at: https://scholars.unh.edu/neigc_trips Recommended Citation Rumble, D. and Chamberlain, C.P., "Graphite Vein Deposits of New Hampshire" (1988). NEIGC Trips. 442. https://scholars.unh.edu/neigc_trips/442 This Text is brought to you for free and open access by the New England Intercollegiate Geological Excursion Conference Collection at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in NEIGC Trips by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. B-7 GRAPHITE VEIN DEPOSITS OF NEW HAMPSHIRE D. Rumble and C. P. Chamberlain Geophysical Laboratory, 2801 Upton Street, N.W..Washington, D.C., 20008 Department of Earth Sciences, Dartmouth College, Hanover, New Hampshire 03755 INTRODUCTION "Black lead (plumbago) is found in large quantities about the grand Monadnock in the township of Jaffrey" (Belknap, 1792, p. 195). So wrote Jeremy Belknap in 1792 of the mountain that dominates the eastern horizon of the 80th Annual NEIGC meeting in Keene, New Hampshire. It is not entirely surprising that the early settlers of New England knew of the value of graphite and were able to recognize it in the field. The graphite mines at Seathwaite in Borrowdale of the English Lake District were worked from the 1600's until the 1830’s yielding a yearly net profit as high as $92,690 in 1803 (Postlethwaite, 1913).