Geology of New England
New England is a region in the North Eastern United States consisting of the states Rhode Island, Connecticut, Massachusetts, New Hampshire, Vermont, and Maine. Most of New England consists geologically of volcanic island arcs that accreted onto the eastern edge of the Laurentian Craton in prehistoric times. Much of the bedrock found in New England is heavily metamorphosed due to the numerous mountain building events that occurred in the region. These events culminated in the formation of Pangaea; the coastline as it exists today was created by rifting during the Jurassic and Cretaceous periods. The most recent rock layers are glacial conglomerates.
Chronology
Overview
The
Archean and Proterozoic eons
In the
.Paleozoic Era
Starting in the
Cambrian Period
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Ordovician Period
During the
Silurian Period
Closure of the Tetagouche-Exploits back-arc in the Early Silurian (430 Ma) accreted the bulk of Ganderia to Laurentia. This event is known as the Salinic Orogeny and was responsible for most of the bedrock that is found in New Brunswick, Newfoundland, and Maine.[4] Examples include the Rangeley sequence found in the Presidential Range that consists of Silurian and Devonian Turbidite sequences, Early Silurian Rangeley Formation, the Middle to Late Silurian Perry Mountain, Smalls Falls, and Madrid Formations.
Devonian Period
The
Carboniferous and Permian periods
The
Mesozoic Era
Triassic Period
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Jurassic Period
New England, like the rest of the eastern United States, does not contain any active volcanoes in the present era. However, the
Cretaceous Period
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Cenozoic Era
Paleogene Period
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Neogene Period
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Quaternary Period
Much of the geomorphology and surficial deposits of New England are a result of glaciation in the Quaternary period. The scoured New England landscape reveals evidence of the
Surficial deposits
The continental ice sheet over New England was more than a mile thick in some places.[11] Grinding and plucking over the landscape created wore down topography and created poorly sorted to well sorted surficial deposits. Large terminal moraines composed of poorly sorted till are present along coasts and can be identified by their thin, patchy, and stony texture.[11] Maine is bordered by moraines that identify the terminus margins of the past ice bodies. The Waldoboro terminal moraine sits on the southeastern coast, while the Highland front moraine parallels the northwestern border. Large continental ice sheets (see Laurentide Ice Sheet) most likely created the large moraines, as it takes time for the long, lumpy ridges to form at a massive scale.[12]
New England is best known for its high density of erratics, which are displaced rocks that differ from the immediate bedrock composition of the region and range from the size of pebbles to boulders. Their surfaces are generally rounded and polished due to rasping.[13] While the bedrock of the area is largely igneous granite, the erratics are sandstone and slate blocks.[12] Sedimentary erratics are visible across the highest peak in Maine, Mount Katahdin.
Erosional processes
The slow and grinding movement of continental ice sheets and alpine glaciers across the landscape creates erosional landforms. Abrasion, plucking, and freeze-thaw action creates the U-shaped valley unique to glacial erosion.
The intense pressure from the ice causes abrasion. This process carves striations, or grooves, into the bedrock as the glacier moves down a slope. Glacial striations help determine the direction of a glacier; visible outcrops in the White Mountains, for instance, indicate ice flow toward the south-southeast.[14] Abrasion also produces rock flour which is visible in glacial outwash plains across New England.
Maine has some of the longest eskers in the world.[12] As the climate began to warm, the glaciers began to melt and drainage from meltwater under the glacier formed huge torrents of sediment that, when compacted, left a long and sinuous ridge or kame. Moose Cave in Grafton Notch is speculated to have been formed in part by a subglacial river.[15] Abol esker in Baxter State Park is a notable serpentine kame.
Kame and kettle topography is commonplace across Maine. Hummocky morphology includes kettle ponds and kettle lakes that are “steep-sided, bowl-shaped depressions in glacial drift deposits"[12] where large blocks of ice melted as the glacier recessed.
Other notable glacial features include cirques, which are visible in mountains such as Mt. Katahdin and Crocker Mountain, indicative of glacial erosion.
Pleistocene Epoch
The
A group of geologists in New England have been using an age-exposure method called the 'Dipstick' Approach, which can determine the rates of ice-sheet thinning and the age of glacially eroded boulder and bedrock surfaces. This approach has been used on various New England mountains, including
Meltwater Pulse 1a
Thinning of the LIS was caused by rapid warming of the Northern Hemisphere produced by a sudden shift towards an interstadial AMOC from 14.6–14.3 ka, a period also known as the Bølling warming.[18] This change in climate caused global sea levels to rise 9–15 m due to deglaciation of Northern Hemisphere ice sheets.[19]
It is uncertain what particular ice sheets contributed the most to the significant sea level rise, but evidence collected from cosmogenic nucleotide dating indicates rapid thinning of the Laurentide Ice Sheet during the Meltwater Pulse 1a (MWP-1A) which could mean the LIS was a main source of glacial meltwater during this time.
The Younger Dryas and Onset of the Holocene
After MWP-1A, around 12.9 ka, the Northern hemisphere experienced a sudden drop in temperatures caused by a reduction in the AMOC towards a stadial mode, which is implicated to be caused by the influx of glacial meltwater from the LIS and is a period known as the Younger Dryas.[20] The AMOC recovered back to an interstadial mode by 11.7 ka which marked the beginning of the Holocene Epoch.[18]
Holocene Epoch
Following the glacial melting of the
The melting of the
References
- ^ a b Marshank, Stephen, 2009, Essentials of Geology, Third Edition, Norton, p. 306-308.
- ^ Hatcher, R. D., 2010, The Appalachian orogen: A brief summary: Geological Society of America Memoirs, v. 206, p. 1-19.
- Raymo, Maureen E.(1989). Written in Stone: A Geologic History of the Northeastern United States. Chester, Connecticut: Globe Pequot.
- ^ Van Staal, C., 2005, The Northern Appalachians: Encyclopedia of geology, v. 4, p. 81-91.
- ^ a b Eusden J. D. Jr., Guzofski, C. A., Robinson, A. C., and Tucker, R. D., 2000, Timing of the Acadian Orogeny in Northern New Hampshire, Journal of Geology, v. 108. p. 219-232.
- ISBN 978-0878422036.
- ^ "Archived copy" (PDF). Archived from the original (PDF) on 2011-07-22. Retrieved 2010-12-10.
{{cite web}}
: CS1 maint: archived copy as title (link) - ^ a b c d "Geology of the White Mountains Part 2: The Mountain Building Events - AMC Outdoors". AMC Outdoors. 2009-02-03. Archived from the original on 2016-10-29. Retrieved 2017-10-20.
- ^ "Tourists Venture Inside a Volcano in New Hampshire". ABC News. 2006-01-07. Archived from the original on 2017-10-21. Retrieved 2017-10-20.
- ^ "Ossipee Mountains in Volcanoes in New Hampshire - Plymouth Portfolio". www.plymouth.edu. Archived from the original on 2017-10-21. Retrieved 2017-10-20.
- ^ )
- ^ a b c d Caldwell, Dabney (1998). Caldwell, D.W., 1998, "Roadside Geology of Maine," Mountain Press Publishing Company, Missoula MT. Mountain Press Publishing Company.
- ISBN 9780393281491.
- ^ Department of Agriculture, Conservation & Forestry, 2002, Glacial and Postglacial Geology Highlights in the White Mountain National Forest, Western Maine: http://digitalmaine.com/cgi/viewcontent.cgi?article=1359&context=mgs_publications Archived 2017-12-02 at the Wayback Machine
- ^ Doughty, A.M., Thompson, W.B., Grafton Notch State Park: Glacial Gorges and Streams under Pressure in the Mahoosic Range, Maine.
- ^ a b Halsted, C.T., Shakun, J.D., Davis, P.T., Bierman, P.R., Corbett, L.B., Koester, A.J., 2018, Mount Greylock as a cosmogenic nuclide dipstick to determine the timing and rate of southeastern Laurentide ice sheet thinning in Grove, Tim and Mango, Helen (editors), Guidebook for field trips in New York and Vermont: New England Intercollegiate Geological Conference, 110th Annual Meeting and New York State Geological Association, 90th Annual Meeting, October 12–14, 2018, Lake George, N.Y., 301 p, color.
- ^ Ivy-Ochs, S., Kerschner, H., Reuther, A., Maisch, M., Sailer, R., Schaefer, J., Kubik, P. W., Synal, H. A. & Schlüchter, CH. (2006): The timing of glacier advances in the northern Alpes based on surface exposure dating with cosmogenic 10Be,26Al, 36Cl and 21Ne. – in: Siame, L.l, Bourlès, D.l. & Brown, E.T. (eds.): In Situ–Produced Cosmogenic Nuclides and Quantification of Geological Processes: Geological Society of America Special Paper, 415: 43–60.
- ^ a b McManus, J.F., FRancois, R., Gherardi, J.M., Keigwan, L.D., Brown-Leger, S., 2004. Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes. Nature 428, 834–837.
- ^ Deschamps, P., Durand, N., Bard, E., Hamelin, B., Camoin, G., Thomas, A.L., Henderson, G.M., Okuno, J.I., Yokoyama, Y., 2012. Ice-sheet collapse and sea-level rise at the Bølling warming 14,600 years ago. Nature 483, 559–564. doi:10.1038/nature10902
- ^ McManus, J.F., Francois, R., Gherardi, J.M., Keigwin, L.D., Brown-Leger, S., 2004. Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes. Nature 428, 834–837.
- ISSN 0705-7199.
- ^ S2CID 129511219.
- ^ ISSN 2055-5563.
- .