Academic literature on the topic 'Earth floor'
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Journal articles on the topic "Earth floor"
Koistinen, Tarja, Leena Ahola, and Jaakko Mononen. "Blue foxes’ (Alopex lagopus) preferences between earth floor and wire mesh floor." Applied Animal Behaviour Science 111, no. 1-2 (May 2008): 38–53. http://dx.doi.org/10.1016/j.applanim.2007.05.011.
Full textAhola, Leena, Tarja Koistinen, and Jaakko Mononen. "Sand Floor for Farmed Blue Foxes: Effects on Claws, Adrenal Cortex Function, Growth and Fur Properties." International Journal of Zoology 2009 (2009): 1–6. http://dx.doi.org/10.1155/2009/563252.
Full textWilson, Scott, Johan Potgieter, and Khalid Mahmood Arif. "Robot-Assisted Floor Surface Profiling Using Low-Cost Sensors." Remote Sensing 11, no. 22 (November 10, 2019): 2626. http://dx.doi.org/10.3390/rs11222626.
Full textLiu, Hao, Pu Wang, Weihe Zhang, Qiang Liu, and Lijun Su. "Comprehensive Measurement of the Deformation and Failure of Floor Rocks: A Case Study of the Xinglongzhuang Coal Mine." Geofluids 2020 (November 12, 2020): 1–14. http://dx.doi.org/10.1155/2020/8830217.
Full textSharma, Arvind, Uttara Kennedy, and Clive Phillips. "A Novel Method of Assessing Floor Friction in Cowsheds and Its Association with Cow Health." Animals 9, no. 4 (March 27, 2019): 120. http://dx.doi.org/10.3390/ani9040120.
Full textCliver, E. W. "The floor in the solar wind: status report." Proceedings of the International Astronomical Union 7, S286 (October 2011): 179–84. http://dx.doi.org/10.1017/s1743921312004814.
Full textChugh, Ashok K. "Influence of valley geometry on stability of an earth dam." Canadian Geotechnical Journal 51, no. 10 (October 2014): 1207–17. http://dx.doi.org/10.1139/cgj-2013-0407.
Full textArpul, Oksana Volodymyrivna, Anastasiya Yuriyivna Spilchuk, and Yuliia Viktorivna Melnyk. "ENERGY FLOOR AS NEW TECHNOLOGY FOR ELECTRICITY EQUIPMENT IN HOTELS OF UKRAINE." GEOGRAPHY AND TOURISM, no. 48 (2019): 74–82. http://dx.doi.org/10.17721/2308-135x.2019.48.74-82.
Full textYahya, N. N., M. Hashim, and S. Ahmad. "Remote Sensing of shallow sea floor for digital earth environment." IOP Conference Series: Earth and Environmental Science 18 (February 25, 2014): 012110. http://dx.doi.org/10.1088/1755-1315/18/1/012110.
Full textHamrouni, Adam, Daniel Dias, and Badreddine Sbartai. "Probabilistic analysis of piled earth platform under concrete floor slab." Soils and Foundations 57, no. 5 (October 2017): 828–39. http://dx.doi.org/10.1016/j.sandf.2017.08.012.
Full textDissertations / Theses on the topic "Earth floor"
Bamberg, Marlene. "Planetary mapping tools applied to floor-fractured craters on Mars." Phd thesis, Universität Potsdam, 2014. http://opus.kobv.de/ubp/volltexte/2014/7210/.
Full textPlanetenforschung umfasst oft zeitintensive Projekte, bei denen Expertise und Erfahrung eine wesentliche Rolle spielen. Auf Grund äusserst komplexer und sich selten wiederholender Forschungsfragen sind Annahmen, Definitionen und Regeln zur Lösung dieser Fragen nicht leicht nachvollziehbar oder aber nicht eindeutig dokumentiert. Ein Vergleich der Ergebnisse unterschiedlicher Forscher zum selben Thema oder eine Erweiterung der Forschungsfrage macht dies somit nur schwer möglich. Vergleiche liefern oftmals verzerrte Ergebnisse, da die Ausgangslage und Randbedingungen unterschiedlich definiert worden sind. Das Ziel dieser Arbeit ist es eine Standardmethode zur Oberflächenanalyse zu entwickeln, die auf zahlreiche Untersuchungsfragen angewandt werden kann. Eine gleichbleibende Qualität der Ergebnisse muss durch diese Methode gewährleistet sein. Ein weiteres Ziel ist es, dass diese Methode ohne Vorwissen und Expertise angewandt werden kann und die Ergebnisse in kurzer Zeit vorliegen. Ausserdem müssen die Ergebnisse vergleichbar und nachvollziehbar sein. Automatisch operierende Analysewerkzeuge können die zahlreichen Anforderungen erfüllen und als Standardmethode dienen. Statistische Ergebnisse werden durch diese Methode erzielt. Die Werkzeuge basieren auf vordefinierten, geowissenschaftlichen Techniken und umfassen Messungen, Berechnungen und Klassifikationen der zu untersuchenden Oberflächenstrukturen. Für die Anwendung dieser Werkzeuge müssen Schlüsselstrukturen und Randbedingungen definiert werden. Des Weiteren benötigen die Werkzeuge eine Datenbank, in der alle Oberflächenstrukturen, aber auch Informationen zu den Randbedingungen gespeichert sind. Es ist mit geringem Aufwand möglich, Datenbanken zu aktualisieren und sie auf verschiedenste Fragestellungen zu adaptieren. Diese Tatsache steigert die Flexibilität, Reproduzierbarkeit und auch Vergleichbarkeit der Untersuchung. Die vordefinierten Randbedingungen und die Qualität der Datenbank haben jedoch auch direkten Einfluss auf die Qualität der Ergebnisse. Um eine gleichbleibend hohe Qualität der Untersuchung zu gewährleisten muss sichergestellt werden, dass alle vordefinierten Bedingungen eindeutig sind und auf vorheriger Forschung basieren. Die automatisch operierenden Analysewerkzeuge müssen als mögliche Standardmethode getestet werden. Hierbei geht es darum Vorteile, aber auch Nachteile zu identifizieren und zu bewerten. In dieser Arbeit werden die Analysewerkzeuge auf einen bestimmten Einschlagskratertyp auf dem Mars angewandt. Krater mit zerbrochenen Kraterböden (Floor-Fractured Craters) sind in verschiedensten Regionen auf dem Mars zu finden, sie zeigen zahlreiche Oberflächenstrukturen und wurden durch unterschiedliche Prozesse geformt. All diese Fakten machen diesen Kratertyp zu einem interessanten und im geologischen und morphologischen Sinne sehr komplexen Anwendungsgebiet. 433 Krater sind durch die Werkzeuge analysiert und je nach Entstehungsprozess klassifiziert worden. Für diese Analyse sind Position der Krater, Art des Umfeldes und Strukturen im Kraterinneren ausschlaggebend. Die kombinierten Informationen geben somit Auskunft über die Prozesse, welche zum Zerbrechen des Kraterbodens geführt haben. Die entwickelten Analysewerkzeuge können geologische Prozesse, die sehr ähnlich zueinander sind, von einander abhängig sind und zusätzlich auch dieselben Oberflächenstrukturen formen, nicht eindeutig unterscheiden. Aus diesem Grund sind fluviale und glaziale Entstehungsprozesse für den untersuchten Kratertyp zusammengefasst. Die Analysewerkzeuge liefern Wahrscheinlichkeitswerte für drei mögliche Entstehungsarten. Um die Qualität der Ergebnisse zu verbessern muss eine Wahrscheinlichkeit über 50 % erreicht werden. Die Werkzeuge zeigen, dass 15 % der Krater durch Vulkanismus, 20 % durch Tektonik und 43 % durch Wasser- und Eis-bedingte Prozesse gebildet wurden. Insgesamt kann für 75 % des untersuchten Kratertyps ein potentieller Entstehungsprozess zugeordnet werden. Für 25 % der Krater ist eine Klassifizierung nicht möglich. Dies kann durch eine Kombination von geologischen Prozessen, einer Überprägung von wichtigen Schlüsselstrukturen, oder eines bisher nicht berücksichtigten Prozesses erklärt werden. Zusammenfassend ist zu sagen, dass es möglich ist planetare Oberflächenstrukturen quantitativ durch automatisch operierende Analysewerkzeuge zu erfassen und hinsichtlich einer definierten Fragestellung zu klassifizieren. Zusätzliche Informationen können durch die entwickelten Werkzeuge erhalten werden, daher sind sie als Assistenzsystem zu betrachten.
Bradley, Christopher R. "Very low frequency seismo-acoustic noise below the sea floor (0.2-10 Hz)." Thesis, Massachusetts Institute of Technology, 1993. http://hdl.handle.net/1721.1/58250.
Full textIncludes bibliographical references (leaves 235-245).
by Christopher Robert Bradley.
Ph.D.
Tentler, Tatiana. "Interaction of Segments along Rifts that Separate Continents and Ridges that Spread Ocean Floors." Doctoral thesis, Uppsala University, Department of Earth Sciences, 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-4134.
Full textThe face of the Earth is constantly renewed by continental rifts that open and allow ridges to spread oceanic floor. Both types of these linear extensional structures are morphologically and structurally segmented. This thesis aims to provide insights into the interaction of such segments as they propagate and mature. It is based on the results of analogue models of evolving rifts and ridges together with field studies of populations of dilational normal faults in the active rift zone of Iceland. Linkage of initially separate segments along rifts and ridges leads to formation of through-going systems operating on a planetary scale. It is argued here that the processes of segment initiation and growth are effectively scale-independent and essentially the same in wide and narrow modes of extension and for shear and dilational failure. Three distinct types of segment coalescence are recognized; these involve tip-to-tip, one tip-to-sidewall and two tips-to-sidewalls segment linkage. The overall structural pattern, particularly the width of the extending domain and the range of displacements and orientations of smaller-scale internal extensional structures, is influenced by both the geometry of extension and the mechanical properties of the extending material. Types of segment linkage appear to be largely independent of localization of dilation or intensity of magmatic accretion. Instead they are controlled mainly by the relative distribution and orientation of interacting segments. A few orders of segmentation along global rift-ridge systems and arrays of dilational normal faults indicate that linear continuous structures accumulate extension in successive increments during which the segments change their geometries in semi-continuous interaction and coalescence.
Grimes, Craig B. "Duration, rates, and patterns of crustal growth at slow-spreading mid-ocean ridges using zircon to investigate the evolution of in situ ocean crust /." Laramie, Wyo. : University of Wyoming, 2008. http://proquest.umi.com/pqdweb?did=1799840381&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Full textVan, Avendonk Hermanus Josephus Antonius. "An investigation of the crustal structure of the Clipperton transform fault area using 3D seismic tomography /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 1998. http://wwwlib.umi.com/cr/ucsd/fullcit?p9823314.
Full textSager, Steven, and sager28@hotmail com. "The Sky is our Roof, the Earth our Floor: Orang Rimba Customs and Religion in the Bukit Duabelas Region of Jambi, Sumatra." The Australian National University. Faculty of Arts, Department of Archeology and Anthropology, 2008. http://thesis.anu.edu.au./public/adt-ANU20091226.232154.
Full textBabcock, Jeffrey Matthew. "Magma chamber structure and Moho reflections along the East Pacific Rise /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 1997. http://wwwlib.umi.com/cr/ucsd/fullcit?p9737307.
Full textŠmardová, Kateřina. "Hliněné povrchy v současné architektuře." Doctoral thesis, Vysoké učení technické v Brně. Fakulta architektury, 2012. http://www.nusl.cz/ntk/nusl-233241.
Full textDeMartin, Brian J. 1976. "Experimental and seismological constraints on the rheology, evolution, and alteration of the lithosphere at oceanic spreading centers." Thesis, Massachusetts Institute of Technology, 2006. http://hdl.handle.net/1721.1/39010.
Full textIncludes bibliographical references (p. 194-197).
Oceanic spreading centers are sites of magmatic, tectonic, and hydrothermal processes. In this thesis I present experimental and seismological constraints on the evolution of these complex regions of focused crustal accretion and extension. Experimental results from drained, triaxial deformation experiments on partially molten olivine reveal that melt extraction rates are linearly dependent on effective mean stress when the effective mean stress is low and non-linearly dependent on effective mean stress when it is high. Microearthquakes recorded above an inferred magma reservoir along the TAG segment of the Mid-Atlantic Ridge delineate for the first time the arcuate, subsurface structure of a long-lived, active detachment fault. This fault penetrates the entire oceanic crust and forms the high-permeability pathway necessary to sustain long-lived, high-temperature hydrothermal venting in this region. Long-lived detachment faulting exhumes lower crustal and mantle rocks. Residual stresses generated by thermal expansion anisotropy and mismatch in the uplifting, cooling rock trigger grain boundary microfractures if stress intensities at the tips of naturally occurring flaws exceed a critical stress intensity factor.
(cont.) Experimental results coupled with geomechanical models indicate that pervasive grain boundary cracking occurs in mantle peridotite when it is uplifted to within 4 km of the seafloor. Whereas faults provide the high-permeability pathways necessary to sustain high-temperature fluid circulation, grain boundary cracks form the interconnected network required for pervasive alteration of the oceanic lithosphere. This thesis provides fundamental constraints on the rheology, evolution, and alteration of the lithosphere at oceanic spreading centers.
by Brian J. deMartin.
Ph.D.
McKnight, Amy R. (Amy Ruth) 1975. "Structure and evolution of an oceanic megamullion on the Mid-Atlantic ridge at 27N̊." Thesis, Massachusetts Institute of Technology, 2001. http://hdl.handle.net/1721.1/59090.
Full textIncludes bibliographical references (leaves 44-48).
Megamullions in slow-spreading oceanic crust are characterized by smooth "turtle-back" morphology and are interpreted to be rotated footwalls of long-lived detachment faults. Megamullions have been analyzed in preliminary studies, but many questions remain about structural and tectonic details of their formation, in particular how the hanging wall develops in conjugate crust on the opposing side of the rift axis. This study compares the structure of an off-axis megamullion complex and its conjugate hanging wall crust on the Mid-Atlantic Ridge near 27 0N. Two megamullion complexes, an older (Ml) and younger (M2), formed successively on the west side of the rift axis in approximately the same location within one spreading segment. Megamullion M1 formed while the spreading segment had only one inside comer on the west flank, and megamullion M2 formed after the segment developed double inside corners west of the axis and double outside corners east of the axis. The older megamullion formed between -22.3 and -20.4 Ma, and the younger megamullion formed between -20.6 and -18.3 Ma; they are presently -200-300 km off-axis. Reconstruction poles of plate rotation were derived and plate reconstructions were made for periods prior to initiation of the megamullion complex (anomaly 6Ar, -22.6 Ma), after the termination of megamullion Ml and during the development of megamullion M2 (anomaly 5E, -19 9 Ma), and shortly following the termination of megamullion M2 (anomaly 5C, -17.6 Ma). These reconstructions were used to compare morphological and geophysical features of both flanks at each stage of the megamullions' development. Megamullion Ml's breakaway occurred at -22.3 Ma and slip along this detachment fault continued and propagated northward at -20.6 Ma to form the northern portion of M2. The exhumed footwall of megamullion M1 has weak spreading-parallel lineations interpreted as mullion structures on its surface, and it forms an elevated plateau between the enclosing segment boundaries (non-transform discontinuities). There was an expansion southward of the detachment fault forming megamullion M2 at -20.1 Ma. It either cut a new detachment fault through megamullion Ml, stranding a piece of megamullion Ml on the conjugate side (east flank), or it linked into the active detachment fault that was forming megamullion M1 or propagated into its hanging wall. The expanded detachment of megamullion M2 and the termination of megamullion M1 occurred during a time when the enclosing spreading segment roughly doubled in length and formed two inside corners. Megamullion M2 developed prominent, high-amplitude (-600 m) mullion structures that parallel the spreading direction for more than 20 km at each inside corner. Its detachment fault was abandoned - 18.6 Ma in the south and ~18.3 Ma in the north ...
by Amy R. McKnight.
S.M.
Books on the topic "Earth floor"
Sea-floor sediment and the age of the earth. El Cajon, Calif: Institute for Creation Research, 1996.
Find full textChudinov, I͡U V. Global eduction tectonics of the expanding earth. Utrecht: VSP, 1998.
Find full textSoundings: The remarkable woman who mapped the ocean floor. New York, NY: Henry Holt and Co., 2012.
Find full textFire under the sea: The discovery of the most extraordinary environment on earth, volcanic hot springs on the ocean floor. New York: Quill W. Morrow, 1991.
Find full textCone, Joseph. Fire under the sea: The discovery of the most extraordinary environment on earth--volcanic hot springs on the ocean floor. New York: Morrow, 1991.
Find full textFire under the sea: The discovery of the most extraordinary environment on earth--volcanic hot springs on the ocean floor. New York: Morrow, 1991.
Find full textVrielynck, Bruno. The changing face of the Earth: The break-up of Pangaea and continental drift over the past 250 million years in ten steps. Paris, France: Commission for the Geological Map of the World, 2003.
Find full textStarkey, Lindsay. Encountering Water in Early Modern Europe and Beyond. NL Amsterdam: Amsterdam University Press, 2020. http://dx.doi.org/10.5117/9789462988736.
Full textEggleston, Jack. Land subsidence and relative sea-level rise in the southern Chesapeake Bay region. Reston: United States Geological Survey, 2014.
Find full textBook chapters on the topic "Earth floor"
Hekinian, Roger. "Our Haven, Planet Earth." In Sea Floor Exploration, 23–51. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-03203-0_2.
Full textSeibold, Eugen, and Wolfgang Berger. "Resources from the Ocean Floor." In Springer Textbooks in Earth Sciences, Geography and Environment, 201–14. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-51412-3_14.
Full textMalinverno, A. "Fractals and Ocean Floor Topography: A Review and a Model." In Fractals in the Earth Sciences, 107–30. Boston, MA: Springer US, 1995. http://dx.doi.org/10.1007/978-1-4899-1397-5_6.
Full textGhosh, Tuhin, and Anirban Mukhopadhyay. "Flood Hazard in Bihar." In SpringerBriefs in Earth Sciences, 1–22. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04438-5_1.
Full textArora, Monohar. "Peak Flood Glacier Discharge." In Encyclopedia of Earth Sciences Series, 827. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_395.
Full textBatista, Celene Milanés. "Coastal Flood Hazard Mapping." In Encyclopedia of Earth Sciences Series, 1–11. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-48657-4_356-1.
Full textBatista, Celene Milanés. "Coastal Flood Hazard Mapping." In Encyclopedia of Earth Sciences Series, 471–80. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93806-6_356.
Full textBarwis, John H. "Flood-Tidal Delta Reservoirs, Medora-Dickinson Trend, North Dakota." In Casebooks in Earth Sciences, 389–412. New York, NY: Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4613-8988-0_17.
Full textMora Chaparro, Juan Carlos. "Identifying and Mapping the Risk of Flood in Urban Areas." In SpringerBriefs in Earth Sciences, 1–22. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-22472-1_1.
Full textDellepiane, Silvana G., and Laura Gemme. "Adaptive SAR Image Processing Techniques to Support Flood Monitoring from Earth Observation Data." In Flood Monitoring through Remote Sensing, 115–34. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-63959-8_6.
Full textConference papers on the topic "Earth floor"
Su, Chao, Lu Wang, and YiJia Dong. "Inverse Analysis on Thermal Parameters of Lock Head Floor Based on BP Neural Network." In Earth and Space 2014. Reston, VA: American Society of Civil Engineers, 2015. http://dx.doi.org/10.1061/9780784479179.059.
Full textNaithani, A. K., Prasnna Jain, Rabi Bhusan, J. K. Jain, and P. C. Nawani. "Geological Mapping of Foundation Floor for Nuclear Building of Rajasthan Atomic Power Project, Rawatbhata, India." In Future Challenges in Earth Sciences for Energy and Mineral Resources. Geological Society of India, 2016. http://dx.doi.org/10.17491/cgsi/2016/95903.
Full textGhaith, Fadi A., and Habib Ur Razzaq. "Thermal Performance of Earth-Air Heat Exchanger Systems for Cooling Applications in Residential Buildings." In ASME 2018 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/imece2018-86974.
Full textJochum, Michael, Gokulakrishnan Murugesan, Kelly Kissock, and Kevin Hallinan. "Low Exergy Heating and Cooling in Residential Buildings." In ASME 2011 5th International Conference on Energy Sustainability. ASMEDC, 2011. http://dx.doi.org/10.1115/es2011-54671.
Full textKusky, Timothy M., Brian F. Windley, and Ali Polat. "FOUR BILLION YEAR RECORD OF OCEAN PLATE STRATIGRAPHY IN ACCRETIONARY OROGENS PRESERVE A RECORD OF SEA FLOOR SPREADING, SUBDUCTION, AND ACCRETION THROUGHOUT EARTH HISTORY." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-308052.
Full textYoshikawa, Hidekazu. "A Proposal on Ultimate Safety Disposal of High Level Radioactive Wastes." In 2013 21st International Conference on Nuclear Engineering. American Society of Mechanical Engineers, 2013. http://dx.doi.org/10.1115/icone21-15117.
Full textYabana, Shuichi, Kenji Kanazawa, Seiji Nagata, Seiji Kitamura, and Takeshi Sano. "Shaking Table Tests With Large Test Specimens of Seismically Isolated FBR Plants: Part 3—Ultimate Behavior of Upper Structure and Rubber Bearings." In ASME 2009 Pressure Vessels and Piping Conference. ASMEDC, 2009. http://dx.doi.org/10.1115/pvp2009-77229.
Full textSchmitz, G., A. Joos, and W. Casas. "Experiences With Thermal Driven, Desiccant Assisted Air Conditioning Systems in Germany." In ASME 2007 International Mechanical Engineering Congress and Exposition. ASMEDC, 2007. http://dx.doi.org/10.1115/imece2007-42192.
Full text"Flood Vulnerability Classification of Lafia Township, Nasarawa State, Nigeria." In International Conference on Earth, Environment and Life sciences. International Institute of Chemical, Biological & Environmental Engineering, 2014. http://dx.doi.org/10.15242/iicbe.c1214016.
Full textMori, M., and T. Kameyama. "GIS analysis of flood damage using Google Earth." In RIVER BASIN MANAGEMENT 2009. Southampton, UK: WIT Press, 2009. http://dx.doi.org/10.2495/rm090101.
Full text