... sedimentation, and shelf bypassing during the Sauk II–Sauk III sea-level fall. Nonfossiliferous dolostones and dolomitic marbles of the proposed carbonate platform correlatives (the Pine Plains Formation in southeastern New York and the Stockbridge Formation from western Massachusetts) also contain common...

... UENPLGALLNAoDNnSgDoIsulnadnd 41° New York Cretaceous Paleogene NEW JERSEY PINE BARRENS 600 m 0 0 20 km area of detail USA 74° 40° N 39o Figure 1. Location of the New Jersey Pine Barrens showing geologic provinces and outcrop of Cretaceous, Paleogene, and Miocene marine and coastal deposits in the coastal plain. Area...

... in the region by open and coastal marine processes. Martinsen et al. (1999) measured several sections in the Ericson Formation at Pine Canyon, Point of Rocks, Tic Canyon, and Cooper Ridge (Pipeline Canyon, loc. 2) around the Rock Springs Uplift ( Fig. 1 ), and identified relatively thin lower delta-plain...

... . CRESSIE , N. 1994 Statistics for spatial data . John Wiley & Sons , New York , 900 pgs. DAVIS , M.B. 1963 On the theory of pollen analysis . American Journal of Science , 261 : 89 – 912 . DAVIS , M.B. , CALCOTE , R.R. , SUGITA , S.S. , and TAKAHARA , H...

... . The identification of the pines of the United States, native and introduced, by needle structure :: New York State College of Forestry , Technical Publication No. 32 , 57 p. Heinrich , H. 1988 . Origin and consequences of cyclic ice rafting in the Northeast Atlantic Ocean during the past 130,000...

... transport on the crustal evolution of the Appalachians. Our study reanalyzed a deep seismic reflection profile across the Pine Mountain window, providing critical new constraints on interpreting the upper crustal structure of the décollement beneath and immediately around the window. The results...

... in a sediment profile from Binnewater Pond, New York, and found the highest charcoal concentration values around 14,000 cal yr BP, when spruce and pine were dominant. After 14,000 cal yr BP, charcoal area concentrations declined for some 4000 years. During this interval, spruce and pine were still present...

... 19,100 and 12,800 BP. Between 12,800 and 9500 BP conifers were rare, and the climate was similar to the northern hardwoods region of western New York State. Pine and oak forest dominated the landscape after 9500 BP, and remained until Western European occupation of the landscape. This rather orderly...

... the Appalachian Basin in northwestern Alabama, broad deep-crustal anomalies of the continental interior include the Grenville front and New York–Alabama lineament (dextral fault). Toward the east and south, high-angle discordance between the northeast-trending Appalachians and the east-west–trending wedge...

... plain. Elongate sedimentary bedforms in the outer shelf bathymetric trough indicate that the West Antarctic Ice Sheet extended to the shelf edge of Pine Island Bay under full-glacial conditions and was drained by an ice stream through this trough ( Figs. 5 and 11 ). The gully-channel network...

... of Seismology , Cambridge University Press , New York . Chen , W. P. , and P. Molnar ( 1983 ). Focal depths of intracontinental and intraplate earthquakes and their implications for the thermal and mechanical properties of the lithosphere , J. Geophys. Res. 88 , 4183 - 4214 . Choy...

..., or, what ails the coastal migration theory : Arctic Anthropology , v. v. 29 pp. 28 ߝ 42 . Erlandson , J.M. , 1994 , Early hunter-gatherers of the California coast : New York , Plenum Pressp . 309 p. Fedje , D.W. , 1993 , Sea levels and prehistory in Gwaii Haanas [M.A. thesis...

.... Buttler , I.W. , and S.J. Riha . 1992 . Water fluxes in Oxisols: A comparison of approaches . Water Resour. Res . 28 : 221 – 229 . Cressie , N.A.C. 1991 . Statistics for spatial data . John Wiley & Sons , New York . Daniels , R.B. , H.J. Kleiss , S.W. Buol...

... fault near Big Pine. Another new late Quaternary fault mapped along the southeastern Owens Lake basin is the Centennial Flat fault, which strikes northwest and parallel to the Owens Valley fault, is west-side-down, and projects northward into Owens Lake playa and southward into the Coso Range (A.S...

... : Elsevier , Amsterdam, New York , p. 1 – 6 . Schmid, A.-M.M. 1979 , Influence of environmental factors on the development of the valve in diatoms : Protoplasma , v. 99 , p. 99 – 115 . Shaw, P.A. 2010 , The use of diatoms as palaeoenvironmental indicators in Botswana...

... feet of Shriver provided there is no New Scotland shale member… The interval of 21 miles between the Pine Creek and Montoursville sections has no Oriskany strata indicated on the State and County geological maps [Oriskany outcrops are present in Williamsport]. Thicknesses, however, at both ends...

... for the Kiowa Cored Well is typical of the Great Plains province. The heat flow contours shown in Figure 1 have been modified from those of Blackwell et al. (1991) to account for this new value. The higher temperatures and geothermal gradient in the Kiowa Cored Well, compared to the Castle Pines well...