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

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Published: 10 December 2022
Last updated: 28 January 2023

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1

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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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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10

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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11

Hawkins, Michael. "Ellenville, New York: A Classic Locality." Rocks & Minerals 82, no. 6 (January 2007): 508–15. http://dx.doi.org/10.3200/rmin.82.6.508-515.

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12

Chamberlain, Steven C., David G. Bailey, George W. Robinson, and Michael Walter. "3 Historic New York Mineral Collectors." Rocks & Minerals 83, no. 3 (May 2008): 220–23. http://dx.doi.org/10.3200/rmin.83.3.220-223.

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13

Lupulescu, Marian. "Tourmaline-Group Minerals from New York State." Rocks & Minerals 83, no. 3 (May 2008): 202–8. http://dx.doi.org/10.3200/rmin.83.3.202-208.

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14

Lupulescu, Marian. "Amphibole-Group Minerals from New York State." Rocks & Minerals 83, no. 3 (May 2008): 210–19. http://dx.doi.org/10.3200/rmin.83.3.210-219.

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15

Davis, John L. "Eurypterus: The State Fossil of New York." Rocks & Minerals 69, no. 4 (August 1994): 251–53. http://dx.doi.org/10.1080/00357529.1994.9925598.

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16

Robinson, George W., and Steven C. Chamberlain. "Gazetteer of Major New York State Mineral Localities." Rocks & Minerals 82, no. 6 (January 2007): 472–83. http://dx.doi.org/10.3200/rmin.82.6.474-483.

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17

Betts, John H. "The Minerals of New York City, Part 1." Rocks & Minerals 84, no. 3 (May 2009): 204–23. http://dx.doi.org/10.3200/rmin.84.3.204-223.

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18

Betts, John H. "The Minerals of New York City, Part 2." Rocks & Minerals 84, no. 3 (May 2009): 224–43. http://dx.doi.org/10.3200/rmin.84.3.224-243.

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19

Robinson, Susan. "William DeRegibus (b. 1954): New York Mining Artist." Rocks & Minerals 80, no. 3 (May 2005): 186–87. http://dx.doi.org/10.3200/rmin.80.3.186-186.

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20

Walter, Michael R. "The Tremolites of St. Lawrence County, New York." Rocks & Minerals 97, no. 2 (March 4, 2022): 142–51. http://dx.doi.org/10.1080/00357529.2022.2004513.

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21

Williams, A. T., N. H. Evans, and S. P. Leatherman. "Genesis of Fire Island foredunes, New York." Sedimentary Geology 42, no. 3-4 (March 1985): 201–16. http://dx.doi.org/10.1016/0037-0738(85)90045-4.

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22

Gradinskaitė, Vilma. "In Search of Missing Collection: The Case of Artist Albert Rappaport." Art History & Criticism 17, no. 1 (November 15, 2021): 31–42. http://dx.doi.org/10.2478/mik-2021-0003.

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Summary The artist Albert Rappaport was born in Anykščiai in 1898. In 1911, the family emigrated to New York. Rappaport became an American citizen in 1925 and began to travel widely. He studied fine art in New York, Paris, Dresden and Munich. He visited South America, Africa and traveled extensively through Europe (1925–1927, 1933, 1937–1939), returning to the United States now and again. The artist participated in several dozen exhibitions. He showed his work in Paris, Rome, Florence, Barcelona, Palma de Mallorca, Copenhagen, Mexico City, Havana, New York, Calgary and Montreal, in addition to his solo exhibitions in 1937 in Warsaw and Vilnius, and in Kaunas, Riga and Tallinn in 1938. After Rappaport’s death, in March 17, 1969 in Montreal, his collection of artworks disappeared and has thus far not been found. To date, two of his painted portraits are known to exist – one belongs to the private collection of Jonathan C. Rappaport, another is on display at the Jewish Public Library in Montreal.
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23

Lupulescu, Marian. "Minerals from the Iron Deposits of New York State." Rocks & Minerals 83, no. 3 (May 2008): 248–66. http://dx.doi.org/10.3200/rmin.83.3.248-266.

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24

Jaszczak, John A., Steven C. Chamberlain, and George W. Robinson. "The Graphites of New York: Scientific and Aesthetic Surprises." Rocks & Minerals 84, no. 6 (October 30, 2009): 502–19. http://dx.doi.org/10.1080/00357520903284848.

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25

Robinson, Susan. "New York City Mineral Artist: Barbara Siegel (b. 1946)." Rocks & Minerals 85, no. 2 (February 17, 2010): 140–45. http://dx.doi.org/10.1080/00357521003591017.

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26

Sutherland, Andrew, Scott Sutherland, George W. Robinson, Marian Lupulescu, David G. Bailey, and Steven C. Chamberlain. "New Danburite Locality Discovered in the Town of Macomb, St. Lawrence County, New York." Rocks & Minerals 92, no. 2 (February 14, 2017): 180–87. http://dx.doi.org/10.1080/00357529.2016.1277924.

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27

Cook, Robert B. "Chondrodite Tilly Foster Mine, Brewster Area Putnam County, New York." Rocks & Minerals 82, no. 6 (January 2007): 484–88. http://dx.doi.org/10.3200/rmin.82.6.484-488.

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28

Walter, Michael, and Steven C. Chamberlain. "Road-Cut Mineral Occurrences of St. Lawrence County New York." Rocks & Minerals 84, no. 3 (May 2009): 254–62. http://dx.doi.org/10.3200/rmin.84.3.254-262.

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29

Walter, Michael, and Steven C. Chamberlain. "Road-Cut Mineral: Occurrences of St. Lawrence County, New York." Rocks & Minerals 80, no. 3 (May 2005): 180–85. http://dx.doi.org/10.3200/rmin.80.3.180-185.

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30

Lupulescu, Marian, Steven C. Chamberlain, Michael Walter, and Scott Wallace. "Diagenetic Uvite with Overgrown DraviteBigelow, St. Lawrence County, New York." Rocks & Minerals 85, no. 3 (April 30, 2010): 250–59. http://dx.doi.org/10.1080/00357529.2010.487359.

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31

Walter, Michael. "An Exogenic Fulgurite Occurrence in Oswego, Oswego County, New York." Rocks & Minerals 86, no. 3 (April 29, 2011): 264–70. http://dx.doi.org/10.1080/00357529.2010.517134.

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32

Walter, Michael R., and George W. Robinson. "The Dafoe Property Minerals, Pierrepont, St. Lawrence County, New York." Rocks & Minerals 94, no. 5 (August 5, 2019): 452–55. http://dx.doi.org/10.1080/00357529.2019.1619139.

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33

LOYDELL, D. K., M. A. KLEFFNER, G. L. MULLINS, A. BUTCHER, D. K. MATTESON, and J. R. EBERT. "The lower Williamson Shale (Silurian) of New York: a biostratigraphical enigma." Geological Magazine 144, no. 2 (February 9, 2007): 225–34. http://dx.doi.org/10.1017/s0016756806003049.

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The lower Williamson Shale at Tryon Park, Rochester, New York State is unique in the co-occurrence of Stimulograptus clintonensis (Hall), previously recorded only from the middle Telychian, and Pterospathodus amorphognathoides amorphognathoides Walliser, previously recorded only from the upper Telychian (Cyrtograptus lapworthi Biozone and higher). These two co-occurring fossils are clearly providing contradictory ages for the lower Williamson Shale. The incorporation of chitinozoan data from both the Williamson and Willowvale shales does not support unequivocally either the graptolite- or conodont-derived biostratigraphy and thus the age of the lower Williamson Shale remains problematical.
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34

McLelland, James, and Jeffrey Chiarenzelli. "Age of Xenolith-Bearing Olivine Metagabbro, Eastern Adirondack Mountains, New York." Journal of Geology 97, no. 3 (May 1989): 373–76. http://dx.doi.org/10.1086/629311.

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35

Hawkins, Michael. "History of the Mineral Collections at the New York State Museum." Rocks & Minerals 82, no. 6 (January 2007): 502–7. http://dx.doi.org/10.3200/rmin.82.6.502-507.

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36

Walter, Michael R., and Geoege W. Robinson. "Mineralogy of the Dafoe Property, Pierrepont, St. Lawrence County, New York." Rocks & Minerals 97, no. 3 (April 26, 2022): 244–53. http://dx.doi.org/10.1080/00357529.2022.2028098.

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37

Walter, Michael R., and Geoege W. Robinson. "Mineralogy of the Dafoe Property, Pierrepont, St. Lawrence County, New York." Rocks & Minerals 97, no. 3 (April 26, 2022): 244–53. http://dx.doi.org/10.1080/00357529.2022.2028098.

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38

Chamberlain, Steven C., and Michael R. Walter. "Collector’s Note: Balmat Mining District Update, St. Lawrence County, New York." Rocks & Minerals 95, no. 5 (August 21, 2020): 463–66. http://dx.doi.org/10.1080/00357529.2020.1744100.

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39

Friedman, Gerald M. "Charles Lyell in New York State." Geological Society, London, Special Publications 143, no. 1 (1998): 71–81. http://dx.doi.org/10.1144/gsl.sp.1998.143.01.07.

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40

Cook, Robert B. "Magnetite:Zinc Corporation of America Mine No. 4, St. Lawrence County, New York." Rocks & Minerals 83, no. 3 (May 2008): 240–47. http://dx.doi.org/10.3200/rmin.83.3.240-247.

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41

Chamberlain, Steven C., Marian Lupulescu, and Ralph Rowe. "Discover of Fluorine-Dominant Dravite Near Gouverneur, St. Lawrence County, New York." Rocks & Minerals 83, no. 4 (July 2008): 320–27. http://dx.doi.org/10.3200/rmin.83.4.320-327.

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42

Bailey, David G., Michael Hawkins, and Charles Hiler. "Minerals of The Silurian Lockport Group Central and Western New York State." Rocks & Minerals 84, no. 4 (July 2009): 326–37. http://dx.doi.org/10.3200/rmin.84.4.326-337.

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43

Helm, Jutta A. "Introduction: German Cities Between Globalization and Unification." German Politics and Society 16, no. 4 (December 1, 1998): 7–17. http://dx.doi.org/10.3167/104503098782486979.

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For more than a century, Germany has had a well-balanced systemof cities showcasing considerable variety in their social and physicalmake-up. It has lacked spectacular global cities like New York,Tokyo, or London. Instead, western cities include industrial citieslike those in the Rhine-Ruhr Valley and cities shaped by universitiesand research (Göttingen or Freiburg), media and publishing (Hamburg),culture and high-technology sectors (Munich), banking andfinance (Frankfurt/Main), wholesale trade and insurance (Cologneand Düsseldorf), as well as government and administration (Berlin,Bonn, and most state capitals). Dramatic social or economic crisesthat generate debates about urban decline have not happened.Thanks in part to effective urban governments, no German city hascome close to the near-collapse of American rustbelt cities duringthe early 1980s, or the fiscal meltdown of New York City in the1970s. Crime has been consistently lower and less violent, and theAmerican racial divide has no equivalent in German cities. East Germancities, while more unevenly developed, have been no less stable.East Berlin was the dominant center, linked to the industrialcities in the North (Rostock) and South (Leipzig, Halle, Dresden) bya rather creaky infrastructure.
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44

Seifert, Karl E., Robert F. Dymek, Philip R. Whitney, and Larry A. Haskin. "Geochemistry of massif anorthosite and associated rocks, Adirondack Mountains, New York." Geosphere 6, no. 6 (December 2010): 855–99. http://dx.doi.org/10.1130/ges00550.1.

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45

Jacobi, Robert D., and John E. Ebel. "Seismotectonic implications of the Berne earthquake swarms west-southwest of Albany, New York." Lithosphere 11, no. 5 (September 6, 2019): 750–64. http://dx.doi.org/10.1130/l1066.1.

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Abstract Five earthquake swarms occurred from 2007 to 2011 near Berne, New York. Each swarm consisted of four to twenty-four earthquakes ranging from M 1.0 to M 3.1. The network determinations of the focal depths ranged from 6 km to 24 km, 77% of which were ≥14 km. High-precision, relative location analysis showed that the events in the 2009 and 2011 swarms delineate NNE-SSW orientations, collinear with NNE trends established by the distribution of the spatially distinct swarms; the events in the 2010 swarm aligned WNW-ESE. Focal mechanisms determined from the largest event in the swarms include one nodal plane that strikes NNE, collinear with the distribution of the swarms and relative events within the swarms. Two, possibly related explanations exist for the Berne earthquake swarms. (1) The swarms were caused by reactivations of proposed blind NE- and NW-striking rift structures associated with the NE-trending Scranton gravity high. These rift structures, of uncertain age (Proterozoic or Neoproterozoic/Iapetan opening), have been modeled at depths appropriate for the seismicity. (2) The NNE-trending swarms were caused by reactivations of NNE-striking faults mapped at the surface north-northeast of the earthquake swarms. Both models involve reactivation of rift-related faults, and the development of the NNE-striking surficial faults in the second model probably was guided by the blind rift faults in the first model. The Berne swarms may be evidence that these faults are seismically capable and, if so, could sustain a maximum event on the order of Mw 5.7–6.6, based on fault segment length.
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46

CRAFT, J. H., and J. S. BRIDGE. "Shallow-marine sedimentary processes in the Late Devonian Catskill Sea, New York State." Geological Society of America Bulletin 98, no. 3 (1987): 338. http://dx.doi.org/10.1130/0016-7606(1987)98<338:sspitl>2.0.co;2.

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47

CARL, JAMES D., WILLIAM F. DELORRAINE, DOUGLAS G. MOSE, and YUCH-NING SHIEH. "Geochemical evidence for a revised Precambrian sequence in the northwest Adirondacks, New York." Geological Society of America Bulletin 102, no. 2 (February 1990): 182–92. http://dx.doi.org/10.1130/0016-7606(1990)102<0182:gefarp>2.3.co;2.

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48

PAIR, DONALD L., and CYRIL G. RODRIGUES. "Late Quaternary deglaciation of the southwestern St. Lawrence Lowland, New York and Ontario." Geological Society of America Bulletin 105, no. 9 (September 1993): 1151–64. http://dx.doi.org/10.1130/0016-7606(1993)105<1151:lqdots>2.3.co;2.

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49

Chamberlain, Steven C. "Tetrahedrite Crystals: From the Zinc Mines at Balmat, St. Lawrence County, New York." Rocks & Minerals 67, no. 3 (June 1992): 176–78. http://dx.doi.org/10.1080/00357529.1992.9926477.

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50

Chamberlain, Steven C., Donald M. Carlin, Michael R. Walter, and David G. Bailey. "Pyrites Mica Mine (Kelly Farm), Town of Canton, St. Lawrence County, New York." Rocks & Minerals 93, no. 4 (June 25, 2018): 337–45. http://dx.doi.org/10.1080/00357529.2018.1454106.

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