... to 2005 due to the availability of PET data from nearby FAWN stations; however, the SWAT model was run for a time period of 1990 to 2005 to ensure adequate “warm up” time for the model to accurately simulate conditions. In this study, all default selections were used for SWAT model parameters...

... of Schoolhouse Member, Maroon Formation. ABA = axial basin anticline, AV = Ashley Valley, DCA = Douglas Creek arch, DHA = Danforth Hills anticline, DJ = Derby Junction, EEC = East Elk Creek, ER = Eagle River, ERC = East Rifle Creek, ES = Elk Springs, FC = Fawn Creek, FLC = Flag Creek, GHM = Grand Hogback...

... in 1968 and several of the other wells (∼5) were drilled in the early 1970s as part of “Operation Reef,” a cooperative exploration project undertaken by Horn River Resources Ltd. The cores examined in this study are 4 to 10 cm in diameter and 7 to 88 m long. The Fawn Lake reef ( Fig. 2 ) is the only reef...

...Vivek S. Kale Abstract Conophytoll cylindricus, Collenia columnaris, Collenia symmetrica and Collenia undosa are reported from the dolomitic intercalations within the Mehdikhera Chertbreccia Formation, exposed in the Choral river valley near Barwah, in Khargoan District, Madhya Pradesh...

... changes are clearly expressed in their morphology and the 'regular sequence of different forms over extensive areas suggests their evolutionary variation. The Fawn Limestone of the Semri Series of Southern Mirzapur exhibits bioherms of Conophyton cylindricus and Collenia columnaris with C. kusiensis...

... the foreland of the orogen overlapping with activity on the Columbia River fault zone, reflecting crustal-scale extension that reached a peak in the Eocene. Samples for 40 Ar/ 39 Ar thermochronology were collected at all structural levels, from a range of rock types. In total, multigrain (and some single...

... outcrop Whit taker (1922) 555.,E~ Fawn Lake reef Distribution of Horn River Formation, types A and B, and related sediments. qP NORTH SOUTH Hay R iver Pm. Waterways Mbr. I . / f ' - - I I I I I I ' . ' I i I I ~ort sio. /¢ . . - , ' - - - r I I / ~ . l ' t I . S lave Po in t Fm. ~- . - . . . '~ - . J...

...) in 1886, 1887 and 1888, traversed the Fawn and Severn Rivers an d areas along the Hudson and James Bay coast ; McInnes (1909, 1912) i n 1903 the Winisk River; and Wilson (1905a, 1905b, 1906a, 1906b, 1909 , 1912) in 1902, 1903, and 1904 the Albany River, its numerous tributarie s in the southwestern corner...

..., muscovite–biotite granite named the Pakeagama Lake pluton ( Breaks et al. 1998 ). The stock, delineated by Stone et al. (1993) and Stone (1998 , Map P.3382), represents one of nine peraluminous granite plutons regionally distributed within the Berens River –Sachigo Subprovince boundary zone...

... concurrently with upper Cheekye fan, as ice diverted meltwater draining the west flank of Mount Garibaldi south along Mashiter Creek into an ice-lateral lake. This lake, formed by ice in Squamish Valley blocking the mouths of Mamquam and Mashiter Valleys, drained south through a bedrock gap into Stawamus River...

... (R=3) Fort Payne (base) 2 E Deicke 2000 2.5–3.0 60–140 <0.25 I-S (R=3) Fort Payne (+14 inches from base) 2 E Deicke 2000 2.5–3.0 60–140 1–2 I-S (R=3), f (tr.) Fort Payne (base) 2 E Deicke 2000 2.5–3.0 60–140 1–2 I-S (R=3), f (tr.) Rising Fawn (Hermitage) 3 E...

... saddle and the majestic Asurchuli, respectively NW and NNW of the township of Pithoragarh. (Fig. 1). PREVIOUS LITERATURE ON STROMATOLITES IN INDIA In India Cryptozoon stromatolites have been reported by Auden (1933) and Mathur and others (1958) from the Fawn limestone of the Semri series of the. THE CALC...

... to use the term ‘Vindhyan’ for the entire group of rocks forming a prominent feature along the northern bank of Narmada river known as Vindhya Parbat or Vindhyachal. The Vindhyan Supergroup is divided into two sequences separated by an unconformity and laterally correlatable conformity ( Bose et al...

.... K. Vopni . The purpose of this coring program was t o find the extent of the reef and what it "roots in" ; that is, its relationship to the Horn River and Lonely Bay formations . A total of 1455 ft of 1 .6 - in diameter core was taken from 5 core-holes designated as Pan A m Fawn Lake core-hole Nos...

... FAWN, Florida Automated Weather Network GLUE, generalized likelihood uncertainty estimation HRU, hydrologic response unit HSPF, Hydrological Simulation Program–FORTRAN IHM, Integrated Hydrologic Model IHM-INTB , Integrated Northern Tampa Bay Hydrologic Model IT, interflow time KsF, saturated...

...R. Anbalagan Abstract Construction of big dams lead to modification of existing fluvial conditions, in addition to affecting the socio-economic conditions of the people of the area. Analysis of the environmental impact on river-bed morphology, hydrogeological regime, stability of hill-slopes around...

... is exposed along the southern flank of the Vindhyan basin in the Son Valley area near the southern bank of the Son river ( Fig. 1 ) and the area under investigation lies between the 24° 27' 10.620" N, 83° 01' 36.749" E as per the topo-sheet number 63P/2 of Survey of India. The Basal Conglomerate lithofacies...

... are inferred to have been triggered in part by climatic changes and, in the case of the two nearest the river, also by associated erosion. Radiocarbon dating indicates that the slides occurred as follows: (a), Scarth's Fields successive rotational slides: Dimlington Stadial–Windermere Interstadial transition...

... streamed down fractures from the River Fal, flowing directly above. Mineralization was marked by torbernite, a bright yellow/green, copper–uranium phosphate. Black pitchblende was intermixed and, below fifty-five metres, it became the sole uranium mineral ( Fawns 1913 : 46–50; Robertson and Dines 1929...