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Mount Marcy

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Journal Article
Published: 01 December 1953
American Mineralogist (1953) 38 (11-12): 1065–1077.
...Howard W. Jaffe Abstract Three small, amygdular camptonite dikes intrude the Marcy anorthosite in Mount Jo, Mount Marcy quadrangle, Essex County, N. Y. They show a northeasterly strike, 80° to 90° dip, and are 13 to 20 inches thick. They are similar to the post-Ordovician camptonite dikes from...
Journal Article
Published: 01 December 1978
American Mineralogist (1978) 63 (11-12): 1116–1136.
...H. W. Jaffe; P. Robinson; R. J. Tracy Abstract Pyroxene-microperthite gneisses associated with anorthosite from the Mount Marcy area contain coexisting iron-rich orthopyroxene, augite, garnet, and hornblende, together with quartz, oligoclase, orthoclase, magnetite and ilmenite. Electron probe...
Image
Panoramic view looking westward toward the Great Range and Mount Marcy near the brink of Roaring Brook Falls at the elevation of ∼500 m. The water-washed exposures start here and continue upstream.
Published: 01 April 2016
Figure 2. Panoramic view looking westward toward the Great Range and Mount Marcy near the brink of Roaring Brook Falls at the elevation of ∼500 m. The water-washed exposures start here and continue upstream.
Image
Mount Marcy apatite fission-track (AFT) age versus elevation plot, including horizontal confined track length distributions.
Published: 01 March 2011
Figure 5. Mount Marcy apatite fission-track (AFT) age versus elevation plot, including horizontal confined track length distributions.
Image
Apatite fission-track (AFT) data (Mount Marcy and Prospect Mountain) plotted against elevation, along with the adjusted position of the Mount Marcy apatite (U-Th)/He (AHe) data using the apparent overlap between the Mount Marcy AFT and AHe ages to constrain the relative position of the AHe profile. The black line depicts a three-stage cooling history.
Published: 01 March 2011
Figure 8. Apatite fission-track (AFT) data (Mount Marcy and Prospect Mountain) plotted against elevation, along with the adjusted position of the Mount Marcy apatite (U-Th)/He (AHe) data using the apparent overlap between the Mount Marcy AFT and AHe ages to constrain the relative position
Journal Article
Published: 01 April 1988
American Mineralogist (1988) 73 (3-4): 261–273.
.... An inverted pigeonite from a pyroxene-bearing quartz syenite gneiss collected in the Mount Marcy quadrangle yields a reintegrated composition of Wo 15.1 En 4.2 Fs 80.7 indicating that igneous crystallization of this rock took place at pressures greater than or equal to approximately 9 kbar. Copyright © 1988...
Journal Article
Journal: GSA Bulletin
Published: 01 February 1980
GSA Bulletin (1980) 91 (2_Part_II): 816–842.
... surfaces) to develop in these rocks. Studies of pyroxenes from the Mount Marcy area indicate that the Precambrian units of the Highlands were subjected to pressures of 7 to 10 kbar (Whitney-and McLelland, 1973; Jaffee and others, 1978; Boone and others, 1978; Bohlen and Essene, 1978). Furthermore...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1916
GSA Bulletin (1916) 27 (1): 645–672.
... New York State probably excels any other equal area of the earth’s surface.” 1 This being so, it is regrettable that the large area occupied by the Adirondacks should still be inadequately shown on our maps of Pleistocene geology. In the central area of this region, especially the Mount Marcy...
Image
Measured (histogram) and calculated (curve) apatite fission-track-length distributions at the 0.05 level, using AFTINV32 (Issler 1996) for samples from the Adirondack High Peaks region: a, Mount Marcy; b, Whiteface Mountain. Model thermal history at 0.05 level using Crowley et al. (1991) annealing model and AFTINV32 (Issler 1996) for samples from the Adirondack High Peaks region: c, Mount Marcy; d, Whiteface Mountain.
Published: 01 March 2000
Figure 2. Measured (histogram) and calculated (curve) apatite fission-track-length distributions at the 0.05 level, using AFTINV32 (Issler 1996 ) for samples from the Adirondack High Peaks region: a , Mount Marcy; b , Whiteface Mountain. Model thermal history at 0.05 level using Crowley et al
Image
Cooling and unroofing rates for four samples from the Adirondack Mountains, New York, based on their apatite fission-track (AFT) and (U-Th)/He ages and respective closure temperatures. High Peak samples include Whiteface Mountain (41), Mount Marcy (42) and Sawteeth Mountain (37); Schroon Lake sample (43) is from the southeastern Adirondacks; 1 σ error bars are indicated for each type of cooling age. The AFT ages for Whiteface, Marcy, and Schroon Lake were previously published in Roden-Tice et al. (2000). Numbers in parentheses correspond to table 1.
Published: 01 September 2005
Figure 7. Cooling and unroofing rates for four samples from the Adirondack Mountains, New York, based on their apatite fission-track (AFT) and (U-Th)/He ages and respective closure temperatures. High Peak samples include Whiteface Mountain (41), Mount Marcy (42) and Sawteeth Mountain (37
Image
(A) Shaded relief map of New York State. Image was derived from GeoMapApp (http://www.geomapapp.org). The inset shows the location of the Adirondacks within the Grenville Province. The eastern Adirondack Mountains and the subregions of interest are outlined. (B) Sampling profile along Prospect Mountain. The location of the Lake George West fault is from Fisher (1984). (C) Sampling profile along Mount Marcy.
Published: 01 March 2011
Prospect Mountain. The location of the Lake George West fault is from Fisher (1984) . (C) Sampling profile along Mount Marcy.
Image
Thermal models constrained using apatite fission-track (AFT) data from the Mount Marcy profile. Samples are presented in the same manner and were modeled using the same parameters as described for Figure 4. Dark gray represents the temperature-time (T-t) region containing paths with a good fit, and light gray represents the T-t region containing paths with an acceptable fit.
Published: 01 March 2011
Figure 7. Thermal models constrained using apatite fission-track (AFT) data from the Mount Marcy profile. Samples are presented in the same manner and were modeled using the same parameters as described for Figure 4 . Dark gray represents the temperature-time ( T-t ) region containing paths
Image
Age versus elevation plot containing both apatite fission-track (AFT) and apatite (U-Th)/He (AHe) ages determined for samples in Mount Marcy profile. The inferred range of possible cooling paths (in gray) and regression lines discussed within the text (solid and dotted lines) are outlined for each data set. Note the apparent overlap of the bottom portion of the AFT profile with the upper portion of the AHe profile, where the region of acceptable cooling paths flattens considerably.
Published: 01 March 2011
Figure 6. Age versus elevation plot containing both apatite fission-track (AFT) and apatite (U-Th)/He (AHe) ages determined for samples in Mount Marcy profile. The inferred range of possible cooling paths (in gray) and regression lines discussed within the text (solid and dotted lines
Journal Article
Journal: GSA Bulletin
Published: 01 March 2011
GSA Bulletin (2011) 123 (3-4): 412–426.
...Figure 5. Mount Marcy apatite fission-track (AFT) age versus elevation plot, including horizontal confined track length distributions. ...
FIGURES
First thumbnail for: Low-temperature thermal history and landscape deve...
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Journal Article
Published: 01 March 2000
The Journal of Geology (2000) 108 (2): 155–169.
...Figure 2. Measured (histogram) and calculated (curve) apatite fission-track-length distributions at the 0.05 level, using AFTINV32 (Issler 1996 ) for samples from the Adirondack High Peaks region: a , Mount Marcy; b , Whiteface Mountain. Model thermal history at 0.05 level using Crowley et al...
FIGURES
First thumbnail for: Evidence for Differential Unroofing in the Adirond...
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Third thumbnail for: Evidence for Differential Unroofing in the Adirond...
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Field observations from landslides within the central Marcy massif (MacKenzie, 2017). (A) Strongly deformed Whiteface-facies anorthosite exposed on the Copper Kiln slide north of Wilmington, New York. (B) Lower-hemisphere projections of foliation measurements and average stretching lineation. (C) Boudinaged coarse-grained gabbro (ortho- and clinopyroxene and plagioclase) with magnetite-bearing leucogranite (based on presence of K-feldspar and quartz) in boudin neck indicating that leucogranite plutonism accompanied boudin formation. (D) Mutually offsetting conjugate shear zones on the Bennies Brook slide located on the northwestern face of Lower Wolfjaw Mountain, with lower-hemisphere projection of mylonitic dike foliations plotted as great circles. (E) East-west–oriented sinistral shear zone in anorthosite in the Bennies Brook slide, with lower-hemisphere projection of shear zones developed within anorthosite plotted as great circles (foliations). (F) Schematic portrayal of conjugate systems and kinematics with average (avg.) stretching lineations from the southeastern margin of the Marcy massif (Fig. 2) and northwestern margin of the Jay–Mount Whiteface unit of the Marcy massif (Fig. 1C) displaying generalized stress orientations.
Published: 08 May 2019
developed within anorthosite plotted as great circles (foliations). (F) Schematic portrayal of conjugate systems and kinematics with average (avg.) stretching lineations from the southeastern margin of the Marcy massif ( Fig. 2 ) and northwestern margin of the Jay–Mount Whiteface unit of the Marcy massif
Journal Article
Journal: Geosphere
Published: 01 April 2016
Geosphere (2016) 12 (2): 572–584.
...Figure 2. Panoramic view looking westward toward the Great Range and Mount Marcy near the brink of Roaring Brook Falls at the elevation of ∼500 m. The water-washed exposures start here and continue upstream. ...
FIGURES
First thumbnail for: The intrusion breccia in the valley of Roaring Bro...
Second thumbnail for: The intrusion breccia in the valley of Roaring Bro...
Third thumbnail for: The intrusion breccia in the valley of Roaring Bro...
Journal Article
Journal: GSA Bulletin
Published: 01 November 2004
GSA Bulletin (2004) 116 (11-12): 1299–1317.
... , Bedrock geology of the High Peaks region, Marcy massif, Adirondacks, New York : Friends of the Grenville Meeting Field Guidebook : Amherst , University of Massachusetts . 78 p. Kemp , J.F. , 1921 , Geology of the Mount Marcy Quadrangle : New York State Museum Bulletin 229 – 230 . 86 p...
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First thumbnail for: Direct dating of Adirondack massif anorthosite by ...
Second thumbnail for: Direct dating of Adirondack massif anorthosite by ...
Third thumbnail for: Direct dating of Adirondack massif anorthosite by ...
Journal Article
Journal: Geosphere
Published: 08 May 2019
Geosphere (2019) 15 (4): 1240–1261.
... developed within anorthosite plotted as great circles (foliations). (F) Schematic portrayal of conjugate systems and kinematics with average (avg.) stretching lineations from the southeastern margin of the Marcy massif ( Fig. 2 ) and northwestern margin of the Jay–Mount Whiteface unit of the Marcy massif...
FIGURES
First thumbnail for: Syn-collisional exhumation of hot middle crust in ...
Second thumbnail for: Syn-collisional exhumation of hot middle crust in ...
Third thumbnail for: Syn-collisional exhumation of hot middle crust in ...
Journal Article
Published: 01 September 2005
The Journal of Geology (2005) 113 (5): 535–552.
...Figure 7. Cooling and unroofing rates for four samples from the Adirondack Mountains, New York, based on their apatite fission-track (AFT) and (U-Th)/He ages and respective closure temperatures. High Peak samples include Whiteface Mountain (41), Mount Marcy (42) and Sawteeth Mountain (37...
FIGURES
First thumbnail for: Regional-Scale Mid-Jurassic to Late Cretaceous Unr...
Second thumbnail for: Regional-Scale Mid-Jurassic to Late Cretaceous Unr...
Third thumbnail for: Regional-Scale Mid-Jurassic to Late Cretaceous Unr...