Bibliografie tematiche / Fill-cut terrace

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Letteratura scientifica selezionata sul tema "Fill-cut terrace"

Autore: Grafiati
Pubblicato: 4 giugno 2021
Ultima modifica: 13 febbraio 2022

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Articoli di riviste sul tema "Fill-cut terrace"

1

Arbogast, Alan F., and William C. Johnson. "Climatic Implications of the Late Quaternary Alluvial Record of a Small Drainage Basin in the Central Great Plains." Quaternary Research 41, no. 3 (May 1994): 298–305. http://dx.doi.org/10.1006/qres.1994.1034.

Testo completo
Abstract (sommario):
AbstractFour late-Quaternary alluvial fills and terraces are recognized in Wolf Creek basin, a small (163 km2) drainage in the Kansas River system of the central Great Plains. Two terraces were created during the late Pleistocene: the T-4 is a fill-top terrace underlain by sand and gravel fill (Fill I), and the T-3 is a strath terrace cut on the Cretaceous Dakota Sandstone. Both Fill II (early Holocene) and Fill III (late Holocene) are exposed beneath the T-2, a Holocene fill-top terrace. The T-1 complex, consisting of one cut and three fill-top terraces, is underlain by Fills III and IV. A po
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2

Norton, K. P., F. Schlunegger, and C. Litty. "On the potential for regolith control of fluvial terrace formation in semi-arid escarpments." Earth Surface Dynamics 4, no. 1 (February 2, 2016): 147–57. http://dx.doi.org/10.5194/esurf-4-147-2016.

Testo completo
Abstract (sommario):
Abstract. Cut–fill terraces occur throughout the western Andes, where they have been associated with pluvial episodes on the Altiplano. The mechanism relating increased rainfall to sedimentation is, however, not well understood. Here, we apply a hillslope sediment model and reported cosmogenic nuclide concentrations in terraces to examine terrace formation in semi-arid escarpment environments. We focus on the Pisco river system in western Peru in order to determine probable hillslope processes and sediment transport conditions during phases of terrace formation. Specifically, we model steady-s
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3

Norton, K. P., F. Schlunegger, and C. Litty. "On the potential for regolith control of fluvial terrace formation in semi-arid escarpments." Earth Surface Dynamics Discussions 3, no. 3 (August 20, 2015): 715–38. http://dx.doi.org/10.5194/esurfd-3-715-2015.

Testo completo
Abstract (sommario):
Abstract. Cut-fill terraces occur throughout the western Andes where they have been associated with pluvial episodes on the Altiplano. The mechanism relating increased rainfall to sedimentation is however not well understood. Here, we apply a hillslope sediment model and reported cosmogenic nuclide concentrations in terraces to examine terrace formation in semi-arid escarpment environments. We focus on the Rio Pisco system in western Peru in order to determine probable hillslope processes and sediment transport conditions during phases of terrace formation. Specifically, we model steady state
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4

Arauza, Hanna M., Alexander R. Simms, Leland C. Bement, Brian J. Carter, Travis Conley, Ammanuel Woldergauy, William C. Johnson, and Priyank Jaiswal. "Geomorphic and sedimentary responses of the Bull Creek Valley (Southern High Plains, USA) to Pleistocene and Holocene environmental change." Quaternary Research 85, no. 1 (January 2016): 118–32. http://dx.doi.org/10.1016/j.yqres.2015.11.006.

Testo completo
Abstract (sommario):
Fluvial geomorphology and stratigraphy often reflect past environmental and climate conditions. This study examines the response of Bull Creek, a small ephemeral creek in the Oklahoma panhandle, to environmental conditions through the late Pleistocene and Holocene. Fluvial terraces were mapped and their stratigraphy and sedimentology documented throughout the course of the main valley. Based on their elevations, terraces were broadly grouped into a late-Pleistocene fill terrace (T3) and two Holocene fill-cut terrace sets (T2 and T1). Terrace systems are marked by similar stratigraphies recordi
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5

Mizutani, Takeshi. "Laboratory experiment and digital simulation of multiple fill-cut terrace formation." Geomorphology 24, no. 4 (September 1998): 353–61. http://dx.doi.org/10.1016/s0169-555x(98)00027-0.

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6

Srivastava, Pradeep, Jayant K. Tripathi, R. Islam, and Manoj K. Jaiswal. "Fashion and phases of late Pleistocene aggradation and incision in the Alaknanda River Valley, western Himalaya, India." Quaternary Research 70, no. 1 (July 2008): 68–80. http://dx.doi.org/10.1016/j.yqres.2008.03.009.

Testo completo
Abstract (sommario):
AbstractWe study the aggradation and incision of the Alaknanda River Valley during the late Pleistocene and Holocene. The morphostratigraphy in the river valley at Deoprayag shows the active riverbed, a cut terrace, and a fill terrace. The sedimentary fabric of the fill terrace comprises four lithofacies representing 1) riverbed accretion, 2) locally derived debris fan, 3) the deposits of waning floods and 4) palaeoflood records. The sedimentation style, coupled with geochemical analysis and Optically Stimulated Luminescence (OSL) dating, indicate that this terrace formed in a drier climate an
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7

Woolfe, Ken J., and Richard G. Purdon. "Deposits of a rapidly eroding meandering river: Terrace cut and fill in the Taupo Volcanic Zone." New Zealand Journal of Geology and Geophysics 39, no. 2 (June 1996): 243–49. http://dx.doi.org/10.1080/00288306.1996.9514708.

Testo completo
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8

Tofelde, Stefanie, Taylor F. Schildgen, Sara Savi, Heiko Pingel, Andrew D. Wickert, Bodo Bookhagen, Hella Wittmann, Ricardo N. Alonso, John Cottle, and Manfred R. Strecker. "100 kyr fluvial cut-and-fill terrace cycles since the Middle Pleistocene in the southern Central Andes, NW Argentina." Earth and Planetary Science Letters 473 (September 2017): 141–53. http://dx.doi.org/10.1016/j.epsl.2017.06.001.

Testo completo
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9

Taillefer, François. "La morphologie des environs de Québec et la basse-vallée du Saint-Laurent." Cahiers de géographie du Québec 2, no. 4 (April 12, 2005): 177–91. http://dx.doi.org/10.7202/020087ar.

Testo completo
Abstract (sommario):
The morphology of the Québec region and the lower St. Lawrence valley is reappraised in this article divided in three parts. The physical landscape is described in part I ; the structural conditions are examined in part II and the morphological problems are presented in part III. The relief is the result of a succession of glacial episodes and submersion and emersion episodes which followed glaciation. The over deepening of the Limoilou depression and the opening of Calvaire lake and Cap Rouge depressions are the results of the glacier. To the submerged phase correspond the alluvial fill, espe
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10

Struik, L. C., P. Schiarizza, M. J. Orchard, F. Cordey, H. Sano, D. G. MacIntyre, H. Lapierre, and M. Tardy. "Imbricate architecture of the upper Paleozoic to Jurassic oceanic Cache Creek Terrane, central British Columbia." Canadian Journal of Earth Sciences 38, no. 4 (April 1, 2001): 495–514. http://dx.doi.org/10.1139/e00-117.

Testo completo
Abstract (sommario):
Upper Paleozoic to Lower Jurassic oceanic rocks of the Cache Creek Terrane near Fort St. James, in central British Columbia, form a stack of thrust sheets cut by steeply dipping strike-slip faults. Paleontologically dated upper Paleozoic strata include bioclastic shallow-water limestone and ribbon chert. Isotopically dated Permian rocks consist of tonalite sills and stocks and rhyolite flows intercalated with basalt flows. Paleontologically dated lower Mesozoic rocks include greywacke, sandstone, siltstone, argillite, ribbon chert, conglomerate, limestone, and basalt tuff. Trembleur Ultramafit
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Più fonti

Tesi sul tema "Fill-cut terrace"

1

Hughes, Matthew William. "Late Quaternary Landscape Evolution and Environmental Change in Charwell Basin, South Island, New Zealand." Phd thesis, Lincoln University. Agriculture and Life Sciences Division, 2008. http://theses.lincoln.ac.nz/public/adt-NZLIU20080214.132530/.

Testo completo
Abstract (sommario):
Charwell Basin is a 6 km-wide structural depression situated at the boundary between the axial ranges and faulted and folded Marlborough Fault Zone of north-eastern South Island, New Zealand. The basin contains the piedmont reach of the Charwell River, and a series of late Quaternary loess-mantled alluvial terraces and terrace remnants that have been uplifted and translocated from their sediment source due to strike-slip motion along the Hope Fault which bounds the basin to its immediate north. The aim of this study was to provide an interdisciplinary, integrated and holistic analysis of late
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2

Hughes, Matthew W. "Late Quaternary landscape evolution and environmental change in Charwell Basin, South Island, New Zealand." Lincoln University, 2008. http://hdl.handle.net/10182/305.

Testo completo
Abstract (sommario):
Charwell Basin is a 6 km-wide structural depression situated at the boundary between the axial ranges and faulted and folded Marlborough Fault Zone of north-eastern South Island, New Zealand. The basin contains the piedmont reach of the Charwell River, and a series of late Quaternary loess-mantled alluvial terraces and terrace remnants that have been uplifted and translocated from their sediment source due to strike-slip motion along the Hope Fault which bounds the basin to its immediate north. The aim of this study was to provide an interdisciplinary, integrated and holistic analysis of late
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