Search results for "Geography"

showing 10 items of 11452 documents

Channel forms recovery in an ephemeral river after gravel mining (Palancia River, Eastern Spain)

2017

[EN] During the 1970s, the Palancia River was intensively affected by gravel mining instream. This activity completely destroyed the fluvial forms, devastating the original wandering pattern. At the end of the 1980s, gravel mining ceased and the river started a process of recovery, only altered by several clearing operations. The aim of this work is to describe these processes of change, analyzing the river's morphosedimentary conditions through a GIS analysis of aerial photographs previous to, simultaneous with, and subsequent to the intense gravel mining activity. Results explain the current difficulties of some ephemeral rivers to recover their original forms, because of the sediment and…

010504 meteorology & atmospheric sciencesHidrologiaFluvial010502 geochemistry & geophysics01 natural sciencesEphemeral riversSedimentsRiver trajectoriesClearing0105 earth and related environmental sciencesEarth-Surface ProcessesHydrologygeographygeography.geographical_feature_categoryLand useEphemeral keySedimentIncisionChannelizedCurrent (stream)Gravel miningLand use changesChannel (geography)GeologyChannel forms
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Comparing flow resistance law for fixed and mobile bed rills

2019

Rills caused by run-off concentration on erodible hillslopes have very irregular profiles and cross-section shapes. Rill erosion directly depends on the hydraulics of flow in the rills, which may differ greatly from hydraulics of flow in larger and regular channels. In this paper, a recently theoretically deduced rill flow resistance equation, based on a power–velocity profile, was tested experimentally on plots of varying slopes (ranging from 9% to 26%) in which mobile and fixed bed rills were incised. Initially, measurements of flow velocity, water depth, cross-section area, wetted perimeter, and bed slope, carried out in 320 reaches of mobile bed rills and in 165 reaches of fixed rills, …

010504 meteorology & atmospheric sciencesHydraulicsfixed bedFlow (psychology)0207 environmental engineering02 engineering and technology01 natural scienceslaw.inventionWetted perimetersymbols.namesakelawFroude numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalirill hydraulic020701 environmental engineering0105 earth and related environmental sciencesWater Science and Technologygeographysoil erosiongeography.geographical_feature_categoryrill flowplot measurementRillFlow conditionsFlow velocitymobile bedsymbolsflow resistanceSediment transportGeologyHydrological Processes
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New insights on secondary minerals from Italian sulfuric acid caves

2018

Sulfuric acid minerals are important clues to identify the speleogenetic phases of hypogene caves. Italy hosts ~25% of the known worldwide sulfuric acid speleogenetic (SAS) systems, including the famous well-studied Frasassi, Monte Cucco, and Acquasanta Terme caves. Nevertheless, other underground environments have been analyzed, and interesting mineralogical assemblages were found associated with peculiar geomorphological features such as cupolas, replacement pockets, feeders, sulfuric notches, and sub-horizontal levels. In this paper, we focused on 15 cave systems located along the Apennine Chain, in Apulia, in Sicily, and in Sardinia, where copious SAS minerals were observed. Some of the…

010504 meteorology & atmospheric sciencesHypogeneQH301-705.5cave minerals speleothem sulfuric acid cave secondary mineralsSettore GEO/04 - Geografia Fisica E GeomorfologiahypogeneGeochemistrySpeleothem010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundCavesulfuric acid caverising watersBiology (General)speleothem0105 earth and related environmental sciencesEarth-Surface Processescave mineralsgeographyCave sulfateSettore GEO/06 - MineralogiaQE1-996.5geography.geographical_feature_categorycave sulfatesSulfuric acidRising waterGeologyhypogene rising waters Apennine Chain mineralogy cave sulfateschemistryApennine Chainmineralogysecondary mineralsGeologyInternational Journal of Speleology
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Reaction path models of magmatic gas scrubbing

2016

Gas-water-rock reactions taking place within volcano-hosted hydrothermal systems scrub reactive, water-soluble species (sulfur, halogens) from the magmatic gas phase, and as such play a major control on the composition of surface gas manifestations. A number of quantitative models of magmatic gas scrubbing have been proposed in the past, but no systematic comparison of model results with observations from natural systems has been carried out, to date. Here, we present the results of novel numerical simulations, in which we initialized models of hydrothermal gas-water-rock at conditions relevant to Icelandic volcanism. We focus on Iceland as an example of a "wet" volcanic region where scrubb…

010504 meteorology & atmospheric sciencesIcelandMineralogychemistry.chemical_elementVolcanism010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationGas phaseHydrothermal systemGeochemistry and PetrologyReaction path0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryEQ3/6GeologyGas emissionsGas-water-rock interactionSulfurMagmatic gas scrubbing; Gas-water-rock interaction; EQ3/6; Hydrothermal systems; IcelandMagmatic gas scrubbingSettore GEO/08 - Geochimica E VulcanologiachemistryVolcano13. Climate actionGeologyData scrubbing
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High time resolution fluctuations in volcanic carbon dioxide degassing from Mount Etna

2014

Abstract We report here on the first record of carbon dioxide gas emission rates from a volcano, captured at ≈ 1 Hz. These data were acquired with a novel technique, based on the integration of UV camera observations (to measure SO2 emission rates) and field portable gas analyser readings of plume CO2/SO2 ratios. Our measurements were performedat the North East crater of Mount Etna, southern Italy, and the data reveal strong variability in CO2 emissions over timescales of tens to hundreds of seconds, spanning two orders of magnitude. This carries importantimplications for attempts to constrain global volcanic CO2 release to the atmosphere, and will lead to an increased insight into short te…

010504 meteorology & atmospheric sciencesLagPlume imagingInduced seismicity010502 geochemistry & geophysicsAtmospheric sciencesPassive degassing01 natural sciencesAtmospherechemistry.chemical_compoundImpact craterGeochemistry and Petrology0105 earth and related environmental sciencesCarbon dioxide; Passive degassing; Plume imaging; Volcanic remote sensing; Volcano seismology; Geophysics; Geochemistry and PetrologyBasaltgeographygeography.geographical_feature_categoryVolcano seismologyPlumeVolcanic remote sensingGeophysicsVolcanochemistryCarbon dioxide13. Climate actionCarbon dioxideCarbon dioxide; Passive degassing; Plume imaging; Volcanic remote sensing; Volcano seismology; Geochemistry and Petrology; GeophysicsSeismologyGeology
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Half a century of forest cover change along the Latvian-Russian border captured by object-based image analysis of Corona and Landsat TM/OLI data

2020

Abstract After 1991, major events, such as the collapse of socialism and the transition to market economies, caused land use change across the former USSR and affected forests in particular. However, major land use changes may have occurred already during Soviet rule, but those are largely unknown and difficult to map for large areas because 30-m Landsat data is not available prior to the 1980s. Our goal was to analyze the rates and determinants of forest cover change from 1967 to 2015 along the Latvian-Russian border, and to develop an object-based image analysis approach to compare forest cover based on declassified Corona spy satellite images from 1967 with that derived from Landsat 5 TM…

010504 meteorology & atmospheric sciencesLand usebusiness.industryIntensive farming0208 environmental biotechnologySoil ScienceGeology02 engineering and technologyLand cover01 natural sciences020801 environmental engineeringGeographyAgricultureAfforestationLand use land-use change and forestryPhysical geographyComputers in Earth SciencesAgricultural productivityScale (map)business0105 earth and related environmental sciencesRemote sensingRemote Sensing of Environment
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Understanding volcanoes in the Vanuatu arc

2016

We report the first helium isotope survey of volcanic gases, hot springs and some olivine phenocrysts along the Vanuatu island arc, from Tanna in the south to Vanua Lava in the north. Low CO2 content and low He-3/He-4 ratios in thermal fluids of Epi (4.0 +/- 0.1 R-a), Efate (4.5 +/- 0.1 R-a) and Pentecost (5.3 +/- 0.5 R-a) islands coherently indicate reduced mantle gas leakage and crustal contamination by radiogenic helium on these extinct volcanic systems of the former (Pliocene) arc. Instead, presently active Vanuatu volcanoes display He-3/He-4 and C/He-3 ratios typical of subduction-related volcanic arcs: He-3/He-4 ratios range from 6.4 +/- 0.5 Ra in southernmost Tanna and 7.23 +/- 0.09 …

010504 meteorology & atmospheric sciencesLavaEarth scienceGeochemistryVanuatu arcHelium isotopes[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesVolcanic fluidsVolcanic GasesGeochemistry and Petrologyevent0105 earth and related environmental sciencesBasaltevent.disaster_typegeographygeography.geographical_feature_categoryVolcanic arcHotspot contributionFumaroleExtinct and active volcanoesMantle sourceSettore GEO/08 - Geochimica E VulcanologiaGeophysicsVolcano13. Climate actionVanuatu arc Volcanic fluids Helium isotopes Extinct and active volcanoes Mantle source Hotspot contributionIsland arcPhenocrystGeology
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Antisana volcano: A representative andesitic volcano of the eastern cordillera of Ecuador: Petrography, chemistry, tephra and glacial stratigraphy

2017

Antisana volcano is representative of many active andesitic strato-volcanoes of Pleistocene age in Ecuador's Eastern Cordillera. This study represents the first modern geological and volcanological investigation of Antisana since the late 1890's; it also summarizes the present geochemical understanding of its genesis. The volcano's development includes the formation and destruction of two older edifices (Antisana I and II) during some 400 + ka. Antisana II suffered a sector collapse about 15,000 years ago which was followed by the birth and growth of Antisana III. During its short life Antisana III has generated >= 50 eruptions of small to medium intensity, often associated with andesitic t…

010504 meteorology & atmospheric sciencesLavaEarth scienceGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesLong-lived evolving andesitic volcanism[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPlagioclaseTephra0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorybiologyAndesitesAndesiteNorthern Volcanic ZoneGeologybiology.organism_classificationVolcano13. Climate actionAntisanaMagmaengineeringPhenocrystGeologyJournal of South American Earth Sciences
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Sustaining persistent lava lakes: Observations from high-resolution gas measurements at Villarrica volcano, Chile

2016

International audience; Active lava lakes – as the exposed upper part of magmatic columns – are prime locations to investigate the conduit flow processes operating at active, degassing volcanoes. Persistent lava lakes require a constant influx of heat to sustain a molten state at the Earth's surface. Several mechanisms have been proposed to explain how such heat transfer can operate efficiently. These models make contrasting predictions with respect to the flow dynamics in volcanic conduits and should result in dissimilar volatile emissions at the surface. Here we look at high-frequency SO2 fluxes, plume composition, thermal emissions and aerial video footage from the Villarrica lava lake i…

010504 meteorology & atmospheric sciencesLavaEarth scienceUAVUV camera010502 geochemistry & geophysics01 natural sciencesElectrical conduitFlux (metallurgy)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPetrologyGeophysic0105 earth and related environmental sciencesgeographyTrail By Firegeography.geographical_feature_categoryTrail ByLava domeFireconduit dynamicPlumeGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGas slugMagmavolcanic degassingGeologyMulti-GAS
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Prodigious emission rates and magma degassing budget of major, trace and radioactive volatile species from Ambrym basaltic volcano, Vanuatu island Arc

2016

Abstract Ambrym volcano, in the Vanuatu arc, is one of the most active volcanoes of the Southwest Pacific region, where persistent lava lake and/or Strombolian activity sustains voluminous gas plume emissions. Here we report on the first comprehensive budget for the discharge of major, minor, trace and radioactive volatile species from Ambrym volcano, as well as the first data for volatiles dissolved in its basaltic magma (olivine-hosted melt inclusions). In situ MultiGAS analysis of H 2 O, CO 2 , SO 2 and H 2 S in crater rim emissions, coupled with filter-pack determination of SO 2 , halogens, stable and radioactive metals demonstrates a common magmatic source for volcanic gases emitted by…

010504 meteorology & atmospheric sciencesLavaGeochemistryMineralogy[SDU.STU]Sciences of the Universe [physics]/Earth SciencesAmbrymVolatile fluxes010502 geochemistry & geophysics01 natural sciencesVolcanic GasesMagma reservoirVanuatuVolatile fluxeGeochemistry and PetrologyCalderaeventGeophysicComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesMelt inclusionsBasaltevent.disaster_typegeographygeography.geographical_feature_categoryMagma degassing budgetStrombolian eruptionGeophysicsVolcano13. Climate actionIsland arcRadioactive disequilibriaGeology
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