Relevant bibliographies by topics / Evolution Canyon

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Evolution Canyon'

Author: Grafiati
Published: 2 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Evolution Canyon"

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Zhang, Shaoyu, Junjiang Zhu, Yonggang Jia, et al. "Submarine Small-Scale Features of Cyclic Steps in the Penghu Canyon: Implications for the Migration of Canyon." Journal of Marine Science and Engineering 10, no. 9 (2022): 1301. http://dx.doi.org/10.3390/jmse10091301.

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The submarine canyons are an important clue to study the evolution process of seafloor geomorphology and they generally indicate the significant linear grooves on the seafloor related to seafloor geodynamic erosion during the evolution of geomorphology. The submarine canyons or canyon groups are not only the channels for the sediment transport from shallow sediments with land-based sources to the deep sea in the sediment source-sink system, but also a key temporary sediment deposition area to study sediment transport patterns and the evolution of submarine geomorphology. In this paper, we proc
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Sun, Meijing, Hongjun Chen, Chupeng Yang, Xiaosan Hu, and Jie Liu. "Multifactorial Controls on the Dongdaobei Submarine Canyon System, Xisha Sea, South China Sea." Journal of Marine Science and Engineering 13, no. 3 (2025): 564. https://doi.org/10.3390/jmse13030564.

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The submarine canyons system is the most widely distributed geomorphic unit on the global continental margin. It is an important concept in the field of deep-water sedimentation and geohazards. Based on high-resolution multibeam bathymetry and two-dimensional seismic data, the dendritic canyon system north of Dongdao island is studied at the eastern Xisha area of the South China Sea. The Dongdaobei submarine canyon is distributed in water depths between 1000 and 3150 m. The main source area in the upper course of the canyon originates from the northwest of Dongdao platform and the Yongxing pla
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Duffy, G. A., T. Horton, and D. S. M. Billett. "Deep-sea scavenging amphipod assemblages from the submarine canyons of the Iberian Peninsula." Biogeosciences Discussions 9, no. 6 (2012): 7831–51. http://dx.doi.org/10.5194/bgd-9-7831-2012.

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Abstract. Submarine canyons have often been identified as hotspots of secondary production with the potential to house distinct faunal assemblages and idiosyncratic ecosystems. Within these deep-sea habitats, assemblages of scavenging fauna play a vital role in reintroducing organic matter from large food falls into the wider deep-sea food chain. Free-fall baited traps were set at different depths within three submarine canyons on the Iberian Margin. Amphipods from the traps were identified to species level and counted. Scavenging amphipod assemblages were compared at different depths within e
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Lin, Ying-Tien, Ling Liu, Biyun Sheng, Yeping Yuan, and Keke Hu. "Laboratory Studies of Internal Solitary Waves Propagating and Breaking over Submarine Canyons." Journal of Marine Science and Engineering 11, no. 2 (2023): 355. http://dx.doi.org/10.3390/jmse11020355.

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This paper carried out laboratory experiments to study evolution of internal solitary waves (ISWs) over submarine canyons with a combination of PIV (particle image velocimetry) and PLIF (planar laser-induced fluorescence) techniques. Taking canyon angle θ and collapse height ∆H as variables, Froude number Fr, head position, energy loss, vorticity field and turbulence intensity when ISWs propagate to the canyon were analyzed. According to the Froude number Fr values, the study cases can be divided into three types: Fr > 1.7 means complete internal hydraulic jump (IHJ); 1 < Fr < 1.7 den
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Lopez-Fernandez, P., S. Bianchelli, A. Pusceddu, A. Calafat, A. Sanchez-Vidal, and R. Danovaro. "Bioavailability of sinking organic matter in the Blanes canyon and the adjacent open slope (NW Mediterranean Sea)." Biogeosciences 10, no. 5 (2013): 3405–20. http://dx.doi.org/10.5194/bg-10-3405-2013.

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Abstract. Submarine canyons are sites of intense energy and material exchange between the shelf and the deep adjacent basins. To test the hypothesis that active submarine canyons represent preferential conduits of available food for the deep-sea benthos, two mooring lines were deployed at 1200 m depth from November 2008 to November 2009 inside the Blanes canyon and on the adjacent open slope (Catalan Margin, NW Mediterranean Sea). We investigated the fluxes, biochemical composition and food quality of sinking organic carbon (OC). OC fluxes in the canyon and the open slope varied among sampling
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Duffy, G. A., T. Horton, and D. S. M. Billett. "Deep-sea scavenging amphipod assemblages from the submarine canyons of the Western Iberian Peninsula." Biogeosciences 9, no. 11 (2012): 4861–69. http://dx.doi.org/10.5194/bg-9-4861-2012.

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Abstract. Submarine canyons have often been identified as hotspots of secondary production with the potential to house distinct faunal assemblages and idiosyncratic ecosystems. Within these deep-sea habitats, assemblages of scavenging fauna play a vital role in reintroducing organic matter from large food falls into the wider deep-sea food chain. Free-fall baited traps were set at different depths within three submarine canyons on the Iberian Margin. Amphipods from the traps were identified to species level and counted. Scavenging amphipod assemblages were compared at different depths within e
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Lopez-Fernandez, P., S. Bianchelli, A. Pusceddu, A. Calafat, A. Sanchez-Vidal, and R. Danovaro. "Bioavailability of sinking organic matter in the Blanes canyon and the adjacent open slope (NW Mediterranean Sea)." Biogeosciences Discussions 9, no. 12 (2012): 18295–330. http://dx.doi.org/10.5194/bgd-9-18295-2012.

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Abstract. Submarine canyons are sites of intense energy and material exchange between the shelf and the deep adjacent basins. To test the hypothesis that active submarine canyons represent preferential conduits of available food for the deep-sea benthos, two mooring lines were deployed at 1200 m depth from November 2008 to November 2009 inside the Blanes canyon and on the adjacent open slope (Catalan Margin, NW Mediterranean Sea). We investigated the fluxes, biochemical composition and food quality of sinking organic carbon (OC). OC fluxes in the canyon and the open slope varied among sampling
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Allen, S. E., C. Vindeirinho, R. E. Thomson, M. GG Foreman, and D. L. Mackas. "Physical and biological processes over a submarine canyon during an upwelling event." Canadian Journal of Fisheries and Aquatic Sciences 58, no. 4 (2001): 671–84. http://dx.doi.org/10.1139/f01-008.

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Short, shelf-break canyons are shown to have a substantial influence on local water properties and zooplankton distribution. Barkley Canyon (6 km long) off the west coast of Vancouver Island was extensively sampled in July 1997 and found to have water property and current patterns similar to those observed over Astoria Canyon (22 km long) off the coast of Washington State. Results from Barkley Canyon reveal that the canyon influence can occur very close to the surface (at the thermocline depth of 10 m) and that, near the canyon rim, the stretching vorticity generated over the canyon is strong
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Nevo, Eviatar. "Evolution of wild barley at “Evolution Canyon”: adaptation, speciation, pre-agricultural collection, and barley improvement." Israel Journal of Plant Sciences 62, no. 1-2 (2015): 22–32. http://dx.doi.org/10.1080/07929978.2014.940783.

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The present paper reviews the state of cultivated barley,Hordeum vulgare, in Old World agriculture and its domestication through its progenitor, wild barley,Hordeum spontaneum. It focuses on the adaptation, incipient sympatric speciation, and domestication ofH. spontaneumin the “Evolution Canyon” model. The “Evolution Canyon,” at lower Nahal Oren, Mount Carmel, Israel, revealsevolution in actionat a microsite caused by interslope microclimatic divergence across life from viruses and bacteria through fungi, plants, and animals including mammals. The interslope adaptive complexes ofH. spontaneum
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Wimmer, Tonya, and Hal Whitehead. "Movements and distribution of northern bottlenose whales, Hyperoodon ampullatus, on the Scotian Slope and in adjacent waters." Canadian Journal of Zoology 82, no. 11 (2004): 1782–94. http://dx.doi.org/10.1139/z04-168.

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A small, apparently isolated, and endangered population of ~130 northern bottlenose whales (Hyperoodon ampullatus Forster, 1770) is found on the Scotian Slope south of Nova Scotia, Canada. Virtually all previous information on these animals had come from the Gully, a large submarine canyon where the northern bottlenose whales can be reliably found. A ship survey along the 1000 m depth contour in 2001 showed northern bottlenose whales only in the Gully, Shortland canyon (50 km east of the Gully), and Haldimand canyon (100 km east of the Gully). Studies in 2002 reconfirmed the presence of the wh
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Dissertations / Theses on the topic "Evolution Canyon"

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Anders, Matt D. "Quaternary Geology and Landscape Evolution of Eastern Grand Canyon, Arizona." DigitalCommons@USU, 2003. https://digitalcommons.usu.edu/etd/6738.

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Tectonics and drainage evolution are controlling overall landscape incision in eastern Grand Canyon. Superimposed on downcutting are dynamic responses of hillslopes, tributary streams, and the Colorado River to glacial-interglacial climate cycles. Five tributary stream fill terraces have been identified, and luminescence dating indicates aggradation was occurring 50- 34 ka {S3), 12-7 ka (S2), and 5-3.5 ka (S1). Seven Colorado River fill terraces have been identified, and luminescence and U-series dating indicate deposition was occurring 343-322 ka (M5), 151-118 ka (M4), and 71-64 ka (M3). Aggr
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Carter, Rachel C. "Submarine Channel Evolution Linked to Rising Salt Dome, Mississippi Canyon, Gulf of Mexico." ScholarWorks@UNO, 2015. http://scholarworks.uno.edu/td/2060.

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By examining halokinetics and channel evolution in a deep-water system, we investigate how submarine channel morphology is affected by changing seascape linked to diapirism. The study area is located in Mississippi Canyon, Gulf of Mexico (GOM), situated directly off the continental slope in a prominent salt dome region. Interactions of salt domes with submarine channels in the GOM are poorly documented. Utilizing 3D seismic data and seismic geomorphology techniques, a long-lived Plio-Pleistocene submarine channel system has been investigated to develop a relationship between variable phases of
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Kapostasy, Daniel Dennis. "Evolution of a Small-Silicic Volcanic Center at Phonolite Hill, Kingston Canyon, Utah." The Ohio State University, 2005. http://rave.ohiolink.edu/etdc/view?acc_num=osu1392815952.

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McOwen, Lisa Kathryn 1968. "The Brock canyon volcanic complex, Grant County, New Mexico: volcanic evolution, alteration, and mineralization." Thesis, The University of Arizona, 1993. http://hdl.handle.net/10150/558223.

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Wald, Laura Cardon. "Structural Analysis of Rock Canyon Near Provo, Utah." BYU ScholarsArchive, 2007. https://scholarsarchive.byu.edu/etd/844.

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A detailed structural study of Rock Canyon (near Provo, Utah) provides insight into Wasatch Range tectonics and fold-thrust belt kinematics. Excellent exposures along the E-W trending canyon allow the use of digital photography in conjunction with traditional field methods for a thorough analysis of Rock Canyon's structural features. Detailed photomontages and geometric and kinematic analyses of some structural features help to pinpoint deformation mechanisms active during the canyon's tectonic history. Large-scale images and these structural data are synthesized in a balanced cross section, w
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Tripsanas, Efthymios. "Evolution of depositional and slope instability processes on Bryant Canyon area, Northwest Gulf of Mexico." Texas A&M University, 2003. http://hdl.handle.net/1969.1/1627.

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Bryant and Eastern Canyon systems are located on the northwest Gulf of Mexico, and they are characterized by a very complex sedimentological history related to glacioeustatic cycles, river discharges, and interactions of depositional and halokinetic processes. Both canyon systems were active during the low sea-level stand of Oxygen Isotope Stage 6, and provided the pathways for the transport of enormous amounts of sediments on the continental slope and abyssal plain of the northwest Gulf of Mexico. Right after their abandonment, at the beginning of Stage 5, salt diapirs encroached into the can
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Martin, Jennifer A. "Debris-Flow Activity in Canyon of Lodore, Colorado: Implications for Debris-Fan Formation and Evolution." DigitalCommons@USU, 2000. https://digitalcommons.usu.edu/etd/6785.

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Large-scale characteristics of Ladore Canyon debris fans are dependent upon the bedrock and lithology of the mainstem and tributary canyons. The largest fans occur in the widest section of the mainstem canyon, which typically correlates with the location of large faults. The steepest fans are found at the mouths of tributaries where cliffs are formed by resistant lithologies. Smaller-scale fan characteristics are dependent upon the magnitude and frequency of events from the respective drainage basin, which is controlled primarily by climate. Three distinct deposit ages ( oldest, intermediate,
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Oguadinma, Vivian Onyinyechukwu. "The submarine canyon heads of the Niger delta : structural controls, sedimentary infilling and Cenozoic evolution." Electronic Thesis or Diss., Université de Lille (2022-....), 2022. http://www.theses.fr/2022ULILR087.

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Les canyons sous-marins sont des corridors majeurs pour le transfert des sédiments des continents vers les bassins sous-marins profonds. Considérés comme des structures de transit scellées par des boues distales, les canyons ont peu fait l'objet de prospective en termes de géologie de réservoir. La source des sédiments, le moment des apports, les mécanismes de transport dans les canyons sous-marins diffèrent d'une marge à l'autre en fonction des contextes climatique et géodynamique, ce qui en fait un vaste champ d'étude. Ce travail présente les résultats d'une étude sismique 3D haute résolutio
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Riter, Joyce Christine Alexis. "Geochemical and tectonic evolution of the Colorado Plateau mantle lithosphere : evidence from Grand Canyon mantle xenoliths /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.

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Tuzlak, Daphnee. "Investigating Patterns of Fluvial Form and Incision Near the Yellowstone Hotspot — Alpine Canyon of the Snake River, Wyoming." DigitalCommons@USU, 2017. https://digitalcommons.usu.edu/etd/5814.

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The Snake River flows across the dynamically uplifting hotspot plume of the Yellowstone region, cuts through the Snake River Range and ultimately enters the lowlying eastern Snake River Plain. Thermal and mantle-dynamic uplift around Yellowstone has been recorded by short-term geodesy and modeled by geophysicists, but measurements over Quaternary timescales and an understanding of how that uplift influences regional incision are absent. The Snake River is the only regional river that crosses the uplifting Yellowstone Plateau and flows into the subsiding eastern Snake River Plain (SRP), and pro
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Books on the topic "Evolution Canyon"

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Robinson, John W. Mt. Goddard: Evolution Basin, Le Conte Canyon, Palasade Crest & vicinity. 3rd ed. Wilderness Press, 1994.

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Chikatunov, V. I. Coleoptera of "Evolution Canyon," Lower Nahal Oren, Mount Carmel, Israel. Pensoft, 1999.

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A, Grout Marilyn, Van Gosen, B. S. 1960-, Hualapai Indian Reservation (Ariz.), and Geological Survey (U.S.), eds. Structural evolution of a Grand Canyon breccia pipe: The Ridenour copper-vanadium-uranium mine, Hualapai Indian Reservation, Coconino County, Arizona. U.S. Dept. of the Interior, Geological Survey, 1988.

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A, Grout Marilyn, Van Gosen, B. S. 1960-, Hualapai Indian Reservation (Ariz.), and Geological Survey (U.S.), eds. Structural evolution of a Grand Canyon breccia pipe: The Ridenour copper-vanadium-uranium mine, Hualapai Indian Reservation, Coconino County, Arizona. U.S. Dept. of the Interior, Geological Survey, 1988.

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Brown, Walter T. In the beginning--. 5th ed. Center for Scientific Creation, 1989.

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T, Brown Walter. In the beginning: Compelling evidence for creation and the flood. 7th ed. Center for Scientific Creation, 2001.

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T, Brown Walter. In the beginning: Compelling evidence for creation and the flood. Center for Scientific Creation, 1996.

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T, Brown Walter. In the beginning: Compelling evidence for creation and the flood. 8th ed. Center for Scientific Creation, 2008.

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Olivier, Buchsenschutz, ed. L' evolution du canton de Levroux d'apre s les prospections et les sondages arche ologiques. Association pour la de fense et l'e tude du canton de Levroux, 1988.

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Olivier, Buchsenschutz, ed. L' Evolution du canton de Levroux d'après les prospections et les sondages archéologiques: Levroux I. Association pour la défense et l'étude du canton de Levroux, 1988.

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Book chapters on the topic "Evolution Canyon"

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Andrews, E. D., Christopher E. Johnston, John C. Schmidt, and Mark Gonzales. "Topographic evolution of sand bars." In The Controlled Flood in Grand Canyon. American Geophysical Union, 1999. http://dx.doi.org/10.1029/gm110p0117.

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Topping, David J., David M. Rubin, Jonathan M. Nelson, Paul J. Kinzel, and James P. Bennett. "Linkage between grain-size evolution and sediment depletion during Colorado River floods." In The Controlled Flood in Grand Canyon. American Geophysical Union, 1999. http://dx.doi.org/10.1029/gm110p0071.

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Yang, Zujun, and Eviatar Nevo. "Heat Shock Proteins in Wild Barley at “Evolution Canyon”, Mount Carmel, Israel." In Heat Shock Proteins and Plants. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-46340-7_5.

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Meyer, Mathias, Jacob Geersen, Sebastian Krastel, Tilmann Schwenk, and Daniel Winkelmann. "Dakar Slide Offshore Senegal, NW-Africa: Interaction of Stacked Giant Mass Wasting Events and Canyon Evolution." In Submarine Mass Movements and Their Consequences. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-2162-3_16.

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Micallef, Aaron, Joshu J. Mountjoy, Miquel Canals, and Galderic Lastras. "Deep-Seated Bedrock Landslides and Submarine Canyon Evolution in an Active Tectonic Margin: Cook Strait, New Zealand." In Submarine Mass Movements and Their Consequences. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-2162-3_18.

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Schoenherr, Tobias. "Why You Cannot Neglect Electronic Procurement." In The Evolution of Electronic Procurement. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-93985-8_2.

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Stanley, Kenneth O., and Joel Lehman. "Case Study 1: Reinterpreting Natural Evolution." In Why Greatness Cannot Be Planned. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-15524-1_10.

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Langdon, John H. "Case Study 24. The Unknowable Biped: Questions We Cannot Answer." In The Science of Human Evolution. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-41585-7_24.

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Hoover, Calvin Bryce. "‘Economic Forces in the Evolution of Civil and Canon Law’." In Law and Economics Vol 2. Routledge, 2024. http://dx.doi.org/10.4324/9781003550143-4.

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Ong, Yen Chin. "Why Hawking Radiation Cannot Be Decoded." In Evolution of Black Holes in Anti-de Sitter Spacetime and the Firewall Controversy. Springer Berlin Heidelberg, 2016. http://dx.doi.org/10.1007/978-3-662-48270-4_5.

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Conference papers on the topic "Evolution Canyon"

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Shukla, Pavan K., Roderick E. Fuentes, Bruce J. Wiersma, Crystal Girardot, Natalie Young, and Theodore Venetz. "Effects of Surface Conditions and Chemistry on Evolution of Open-Circuit Potential of Carbon Steel in Nuclear Waste Simulants." In CORROSION 2020. NACE International, 2020. https://doi.org/10.5006/c2020-14841.

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Abstract Several million gallons of high-level radioactive waste is stored in underground carbon-steel storage tanks at the Hanford site. The waste chemistries are complex mixture of organic and inorganic species and are predominantly alkaline. Carbon steel is expected undergo passive dissolution under the alkaline conditions, but certain corrosive species in the waste chemistries such as chloride and nitrate could cause pitting corrosion and stress corrosion cracking (SCC). The risk of pitting corrosion is determined using cyclic potentiodynamic polarization (CPP) tests and by estimating pitt
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Michel, James H., Carol Powell, Ivan Richardson, and Bopinder Phull. "Development of Copper Alloys for Seawater Service from Traditional Application to State-of-the Art Engineering." In CORROSION 2017. NACE International, 2017. https://doi.org/10.5006/c2017-09382.

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Abstract Since antiquity both wrought and cast forms of copper alloys have exhibited significant corrosion resistance in marine environments. Their properties have been developed and modified over the years to meet today’s exacting engineering challenges and continue to offer solutions to a range of industries requiring reliability in seawater including commercial and naval shipbuilding, offshore seawater-handling and firewater systems, and thermal desalination plants. This paper describes the range of copper alloys in marine service today and the evolution of applications which include ships'
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Case, Raymundo, and Manuel Gonzalez. "Fracture Toughness Assessment of the Susceptibility for Sulfide Stress Corrosion Cracking in High Strength Carbon and Low Alloy Steels: a Review." In CORROSION 2018. NACE International, 2018. https://doi.org/10.5006/c2018-10851.

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Abstract High strength carbon steels typically used as oil country tubular goods can be susceptible to sulfide stress corrosion cracking (SSC) when in service in environments that contain H2S. In the last 25 years, linear-elastic fracture mechanics has been used to understand both the mechanistic aspects of this form of cracking and to quantify the susceptibility to SSC of different OCTG steel grades. This paper presents a review on the evolution of the Double Cantilever Method (DCB) as a standard practice to assess the threshold stress intensity parameter (KISSC), evaluating the capabilities
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Bazzoni, Bruno, and Luciano Lazzari. "The Lateral Gradient Technique for Potential Measurements in Presence of Stray Current." In CORROSION 1996. NACE International, 1996. https://doi.org/10.5006/c1996-96202.

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Abstract In presence of stray current, the potential measurement is inevitably affected by strong spurious ohmic drop contribution, which cannot be eliminated by ordinary techniques, such as the well known on/off one. The “lateral gradient technique” appeared, from the theoretical standpoint, very attractive, being easy and fast. Rather than to give the true protection potential conditions, the power of the method rely on the information on over protection conditions; this has to be avoided in order to not damage the protection coating and to exclude hydrogen evolution. After a brief introduct
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Катлине Коблев, А., A. Katline Koblev, С. Лещенко, S. Leschenko, К. Макаров, and K. Makarov. "GROUNDSWELL OF COLLAPSING WAVES TO THE COAST IN THE ZONES OF SUBMARINE CANYONS." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce3aa18dd48.92889782.

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Short characteristics of submarine canyons located between the rivers Mzymta and Psou and supervisions for their dynamics and influence on coastal constructions are examined in this report. The scheme of an underwater canyon with the directions of wave beams, the line of collapse of waves, their border groundswell to the coast and coastal constructions is presented. It is suggested to define an altitude of the length of
 groundswell of collapsing waves to the coast on the basis of the law of energy conservation of surfy waves. The detailed calculating procedure taking into account a rough
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Young, Richard A. "COMPARATIVE LANDSCAPE EVOLUTION IN THE WESTERN GRAND CANYON REGION, ARIZONA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-280124.

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Петров, В., V. Petrov, Н. Ярославцев, and N. Yaroslavcev. "COASTAL PROCESSES IN ZONE OF UNDERWATER CANYONS ON INTERFLUVIAL AREA OF MSYMTA AND PSOU RIVERS." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce3d261c170.40774587.

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There is considered dynamics of the shore between the Msymta and Psou rivers. It is shown that the loss of sediments more than solid runoff of Msymta river. The deficit is compensated by erosion of pebble beaches on the area from canyon «Novy» to the cape «Konstantinivski».
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Jensen, Austin, Elizabeth Balgord, Alexander Berniche, Katherine E. Potter, Skadi Kobe, and Adolph Yonkee. "PETROTECTONIC EVOLUTION OF THE PRECAMBRIAN FARMINGTON CANYON COMPLEX OF NORTHERN UTAH." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359687.

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Лещенко, С., S. Leschenko, А. Катлине Коблев, and A. Katline Koblev. "ANALYSIS OF BANK PROTECTION MEASURES CANYON IN THE COAST OF NEW IMERETI VALLEY IN THE ADLER DISTRICT OF SOCHI." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce3d0199488.77738502.

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The Imeretinsky lowland – the central fragment of a large Black Sea terrace of the Caucasian coast of Russia, is located in interfluve the rivers Mzymty and Psou. In its central and western part large sports complexes of the winter Olympic Games "Sochi-2014" and the Olympic village are under construction. It has led to necessity of engineering protection of coast from the constructed port Imeretinsky to east board of cape of Konstantinovsky.
 In the report the site located from the Southern pier of port to the western board of cape of Konstantinovsky is considered. On a site the underwate
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Okhai, Disha, Madeline Lewis, Joel DesOrmeau, Ayla Pamukcu, and Michael Eddy. "EVOLUTION OF THE IXL-JOB CANYON MAGMATIC SYSTEM IN THE STILLWATER RANGE, NV." In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-391575.

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Reports on the topic "Evolution Canyon"

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King, E. L. Canyon-head evolution and the influence of glacial regime along the southeast Canadian margin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/295689.

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Karlstrom, Karl, Laura Crossey, Allyson Matthis, and Carl Bowman. Telling time at Grand Canyon National Park: 2020 update. National Park Service, 2021. http://dx.doi.org/10.36967/nrr-2285173.

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Grand Canyon National Park is all about time and timescales. Time is the currency of our daily life, of history, and of biological evolution. Grand Canyon’s beauty has inspired explorers, artists, and poets. Behind it all, Grand Canyon’s geology and sense of timelessness are among its most prominent and important resources. Grand Canyon has an exceptionally complete and well-exposed rock record of Earth’s history. It is an ideal place to gain a sense of geologic (or deep) time. A visit to the South or North rims, a hike into the canyon of any length, or a trip through the 277-mile (446-km) len
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Tran, Tut, Alexandra Bonham, Justin Tweet, and Vincent Santucci. Bryce Canyon National Park: Paleontological resource inventory. National Park Service, 2024. http://dx.doi.org/10.36967/2302804.

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Originally designated as a national monument in 1923, Bryce Canyon National Park (BRCA) is recognized for its exceptional pink-orange hoodoo landscapes. Its iconic hoodoos, consisting of the Paleocene?Eocene Claron Formation, are only part of the geology of BRCA, which includes a nearly uninterrupted sequence of Late Cretaceous Western Interior Seaway evolution and diverse depositional environments from approximately 100 to 77 million years ago. This sequence consists of the coastal Naturita Formation, the marine Tropic Shale, the transitional Straight Cliffs Formation, and the terrestrial Wah
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Tran, Tut, Alexandra Bonham, Justin Tweet, and Vincent Santucci. Bryce Canyon National Park: Paleontological resource inventory (public version). National Park Service, 2024. http://dx.doi.org/10.36967/2303710.

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Originally designated as a national monument in 1923, Bryce Canyon National Park (BRCA) is recognized for its exceptional pink-orange hoodoo landscapes. Its iconic hoodoos, consisting of the Paleocene?Eocene Claron Formation, are only part of the geology of BRCA, which includes a nearly uninterrupted sequence of Late Cretaceous Western Interior Seaway evolution and diverse depositional environments from approximately 100 to 77 million years ago. This sequence consists of the coastal Naturita Formation, the marine Tropic Shale, the transitional Straight Cliffs Formation, and the terrestrial Wah
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Isom, Shelby. Compositional and Physical Gradients in the Magmas of the Devine Canyon Tuff, Eastern Oregon: Constraints for Evolution Models of Voluminous High-silica Rhyolites. Portland State University Library, 2000. http://dx.doi.org/10.15760/etd.5773.

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Schofield, Ian S., Paul L. Brown, Mark J. Logsdon, and Matthew P. Wickham. Waste Rock Dump Characterization Studies at the Bingham Canyon Mine. Utah Geological Survey, 2024. http://dx.doi.org/10.34191/mp-179.

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The Bingham Canyon Mine, located near Salt Lake City, Utah, is surrounded by more than 6 billion tons of waste rock developed over the open cut mining history from 1903 to present; the surface area of the waste rock is approximately 5000 acres. Waste rock dumps have a thickness of more than 1 200 feet from crest to toe. From 1930 to 2000, selected portions of the waste rock dumps were commercially leached using a ferric-sulfate-based lixiviant to extract copper, whereas other portions have only received meteoric leaching. From 2011 to present, Rio Tinto Kennecott has studied the evolution and
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Lianos, Vasilis. Automation and Artificial Intelligence in the possible transition to a postcapitalist society. Mέta | Centre for Postcapitalist Civilisation, 2023. http://dx.doi.org/10.55405/mwp17en.

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Throughout history, technology and its evolution have significantly impacted the societal modes of production and organisation. The highest rise in technological evolution has been observed under the capitalist system. Technology has not, as of yet, proved to be capitalism’s demise. However, some believe that advances in Artificial Intelligence and automation render them radically different technologies to those of the past and will mean capitalism’s demise and the dawn of a new, postcapitalist era. This paper will assess this claim by looking at historical evidence and contemporary theoretica
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O’Dea, Annika, and Katherine Brodie. Analysis of beach cusp formation and evolution using high‐frequency 3D lidar scans. Engineer Research and Development Center (U.S.), 2024. http://dx.doi.org/10.21079/11681/48781.

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Beach cusp characteristics were explored using 15 months of 3D lidar scans collected hourly at the Duck, NC, Field Research Facility. Fourier analyses performed on lidar-derived beach elevation contours generated spatial cusp spectra. Active cusp events identified from the location and magnitude of each spectrum’s peak were used to evaluate conditions during cusp formation and evolution. Cusps primarily developed during normally-incident, long-period, low-energy wave conditions with low frequency spread and reflective beach conditions. Often, however, persistent upper-beach cusps lasted days t
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Leissem, Andreas, Volker Schwinn, Rolf K. Poepperling, and Jean-Pierre Jansen. IPC-04-01 Concepts and Production Results of Heavy Wall Linepipe in Grades up to X70 for Sour Service. Pipeline Research Council International, Inc. (PRCI), 2002. http://dx.doi.org/10.55274/r0011827.

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This paper summarizes the main mechanism and influencing factors for Hydrogen Induced Cracking. The evolution of HIC test requirements over nearly 30 years for linepipe intended for sour service is reviewed. Some typical examples of the requirements for sour service pipe production at Europipe (formerly Mannesmann) developed over the past 20 years and the details of trial production of sour service pipes in grade X 70 with 30 mm wall thickness are presented. However, with the steadily increasing demands, it becomes progressively more difficult to fulfill the before mentioned standard test cond
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Samet, Andrew. Labor Provisions in the U.S Free Trade Agreements: Case Study of México, Chile, Costa Rica, El Salvador and Peru. Inter-American Development Bank, 2011. http://dx.doi.org/10.18235/0008420.

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This document is divided into two components. First, it provides a comparison of the obligations contained under these four agreements and presents the evolution in the language and commitments in them for the 15 year period between 1993 and 2008 during which they were negotiated. Second, it reviews the developments in each country during the relevant period with regard to changes in labor laws and regulations, and also in the strengthening of labor institutions 2 relevant for labor law enforcement, specifically the ministries of labor and the labor justice systems. This document cannot assess
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