Bog Turtle Habitat on the Lake Ontario Coastal Plain of New York State

2010 ◽  
Vol 17 (3) ◽  
pp. 415-436 ◽  
Author(s):  
Peter A. Rosenbaum ◽  
Andrew P. Nelson
Keyword(s):  
New York ◽  
Coastal Plain ◽  
New York State ◽  
Lake Ontario ◽  
York State ◽  
Bog Turtle

scholarly journals Consumption of Lake Ontario sport fish and the incidence of colorectal cancer in the New York State Angler Cohort Study (NYSACS)

2017 ◽  
Vol 154 ◽  
pp. 86-92 ◽  
Author(s):  
Catherine L. Callahan ◽  
John E. Vena ◽  
Joseph Green ◽  
Mya Swanson ◽  
Lina Mu ◽  
...  
Keyword(s):  
Colorectal Cancer ◽  
New York ◽  
Cohort Study ◽  
New York State ◽  
Lake Ontario ◽  
York State ◽  
Sport Fish

Source parameters of the June 13, 1967 earthquake near Lake Ontario, New York State

1977 ◽  
Vol 14 (11) ◽  
pp. 2651-2657 ◽  
Author(s):  
Michio Hashizume ◽  
Nagakoto Tange
Keyword(s):  
New York ◽  
Surface Wave ◽  
Epicentral Distance ◽  
Source Parameters ◽  
New York State ◽  
Focal Depth ◽  
Lake Ontario ◽  
Strike Slip ◽  
York State ◽  
Long Period

Source parameters of an earthquake with magnitude mb = 4.4 were determined by using surface waves. Small but clear surface wave signals were observed on long period records gathered from seismograph stations within an epicentral distance of about 2000 km. The focal mechanism was determined to be of strike-slip type with the maximum and the minimum compression axes trending NNW–SSE and ENE–WSW, respectively. The focal depth was determined to be near either 3 or 20 km.

I.—Glacial Geology of Western New York

1897 ◽  
Vol 4 (12) ◽  
pp. 529-537
Author(s):  
Herman Le Roy Fairchild
Keyword(s):  
New York ◽  
New York State ◽  
Lake Ontario ◽  
Glacial Geology ◽  
York State ◽  
Upper Silurian ◽  
East And West ◽  
North And South

The area herein described is that part of New York State lying south of Lake Ontario, and west of longitude 76°. The dimensions of the area are, approximately, 95 miles north and south and 155 miles east and west, or nearly 15,000 square miles. The rocks are shales, sandstones, and limestones of the Upper Silurian and Devonian systems. The strike is nearly east and west, with a southward dip averaging perhaps 50 feet to the mile.

scholarly journals Consumption of Contaminated Sport Fish from Lake Ontario and Time-to-Pregnancy: New York State Angler Cohort

1997 ◽  
Vol 146 (11) ◽  
pp. 949-954 ◽  
Author(s):  
G. M. Buck ◽  
L. E. Sever ◽  
P. Mendola ◽  
M. Zielezny ◽  
J. E. Vena
Keyword(s):  
New York ◽  
New York State ◽  
Lake Ontario ◽  
Time To Pregnancy ◽  
York State ◽  
Sport Fish

scholarly journals Structural Elements and Neotectonics of Prince Edward County, Southern Ontario

2007 ◽  
Vol 47 (3) ◽  
pp. 303-312 ◽  
Author(s):  
Gail H. McFall
Keyword(s):  
New York ◽  
New York State ◽  
Lake Ontario ◽  
Structural Features ◽  
Structural Elements ◽  
Southern Ontario ◽  
York State ◽  
Salmon River ◽  
Middle Ordovician ◽  
Prince Edward County

ABSTRACT The seismically active Clarendon-Linden Fault of western New York State appears to connect with the Salmon River Fault and possibly with the Picton Fault, both of which cut through Prince Edward County, southern Ontario. Bedrock exposures display a variety of structural features including faults, fractures, and pop-ups which indicate that the region has been subjected to repeated tectonism since the Middle Ordovician. Thus, despite the general perception that Prince Edward County and the rest of the Lake Ontario region is one of low seismic potential, geological and geophysical data suggest otherwise.

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