Search results for "alluvial"

showing 10 items of 31 documents

Structure and evolution of a Messinian mixed carbonate-siliciclastic platform: the role of evaporites (Sorbas Basin, South-east Spain).

2010

36 pages; International audience; The Sorbas Member is a late Messinian complex sedimentary systemthat formed immediately following deposition of the Messinian evaporites in the Sorbas Basin (South-east Spain). This work describes the sequence architecture and facies organization of a continuous kilometre long, alluvial fan to open platform transect near the village of Cariatiz in the north-east of the basin. The postevaporitic Cariatiz platform was a mixed carbonate-siliciclastic system composed of four intermediate-frequency, fifth-order depositional sequences (Depositional Sequences 1 to 4) arranged in an overall prograding trend. The intense fracturing and brecciation of these deposits …

010506 paleontologyEvaporiteStratigraphy[SDE.MCG]Environmental Sciences/Global Changeslate Messinian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentPaleontologyooidsooids.14. Life underwater0105 earth and related environmental sciencesmixed carbonate/siliciclastic platform[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryAlluvial fanmicrobialitesGeology[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/Tectonics15. Life on landEvaporite collapse and deformation[ SDE.MCG ] Environmental Sciences/Global Changes[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesOoidSiliciclasticSedimentary rockProgradationGeology
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Discovery of an Autunian macroflora and lithostratigraphic re-investigation on the western border of the Lodève Permian basin (Mont Sénégra, Hérault,…

2013

11 pages; International audience; Re-investigation of the western edge of the Lodève basin allows reassignment of one sandstone-conglomerate formation previously identified as "terminal Stephanian" to Early Autunian. The existence of two unconformable (Stephanian and Autunian) megasequences, separated by a sedimentary gap, which had been rejected, is thus re-affirmed. The authors also found, less than 20 m above the basal Autunian conglomerate, a macroflora with taxa characteristic of the famous Tuilières flora from a site, located in the eastern part of the basin near Lodève, in the Grey Autunian group. This confirms that the new Mont Sénégra fossiliferous beds belong to the Lower Autunian…

010506 paleontologyFloodplainPeltaspermesContext (language use)Structural basin010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesConglomerate[ SDE ] Environmental SciencesPaleontologyMacrofloraGroup (stratigraphy)ConiférophytesAssélien0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographygeography.geographical_feature_categoryGeneral EngineeringAlluvial fanStéphanien[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDE]Environmental SciencesSedimentary rockAutunien basalDiscordance sédimentaire[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Landscape reconstruction and major flood events of the River Main (Hesse, Germany) in the environs of the Roman fort at Groβkrotzenburg

2020

Abstract Detailed geoarchaeological studies were conducted at the Groβkrotzenburg floodplain (Southern Hesse, Germany) in order to reconstruct the fluvial palaeogeography and search for Roman harbour installations. Another objective was to reconstruct the local flood history based on stratigraphic and geochronological data. Prospection based on electrical resistivity tomography, vibracoring and direct push electrical conductivity logging were carried out to detect and analyze subsurface stratigraphies. Altogether, 6 sediment cores, up to 7 m long, were drilled along transects along and perpendicular to the present course of the River Main. Based on sedimentological and geochemical data, we …

010506 paleontologygeographygeography.geographical_feature_categoryFloodplainFlood mythWater flowBedrockFluvial010502 geochemistry & geophysics01 natural sciencesAlluvial plainSedimentary rockPhysical geographyPalaeogeographyGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary International
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Diplurans of subsurface terrestrial habitats in the Iberian Peninsula, with a new species description (Diplura: Campodeidae)

2017

Although Iberian subsurface terrestrial habitats have been sampled for a half century, they remain poorly known. During the last five years much more sampling of these subsurface habitats has been made, mainly in scree slopes (also called colluvial Mesovoid Shallow Substratum habitats, MSS) but also in alluvial debris of temporal watercourses (alluvial MSS). In our study, diplurans, a basal hexapod group, were extracted from two hundred traps installed in 69 locations in the mountain ranges of six different regions of the Iberian Peninsula, from north to south: Cantabrian, Pyrenees, Iberic System, Central System, Prebaetic and Penibaetic Mountains. A total of 1251 specimens in fifteen diplu…

0106 biological sciencesArthropodaAlluvial MSS habitatsEcology010607 zoologyHexapodaBiologybiology.organism_classificationDiplura010603 evolutionary biology01 natural sciencesHexapodaSpecies descriptionColluvial MSS habitatsMesovoid Shallow SubstratumHabitatCampodeidaeCampodeaScreeAnimal Science and ZoologyAlluviumDipluraScree slope faunaEcology Evolution Behavior and SystematicsTaxonomy
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Early response ofQuercus roburseedlings to soil compaction following germination

2018

Logging operations using heavy machinery effect changes in soil characteristics due to compaction; such conditions can negatively influence seedling development. In stands managed on the basis of close-to-nature silviculture or continuous cover forestry, successful establishment of natural regeneration after logging is important to ensure the proper functioning of a forest ecosystem, to promote soil recovery, and to prevent and mitigate land degradation processes (such as soil erosion, mudflow, waterlogging, and landslides) related to soil compaction and rutting. This work aimed to assess the early response of Quercus robur seedlings to soil compaction during the first 1.5 months after germ…

0106 biological scienceslogging operationSoil ScienceRoot systemDevelopment01 natural sciencesseedling growthQuercus roburAlluvial soilsEnvironmental Chemistrypedunculate oakSettore AGR/06 - Tecnologia Del Legno E Utilizzazioni ForestaliSilvicultureGeneral Environmental Sciencebiology04 agricultural and veterinary sciencesbiology.organism_classificationHorticulturePlant developmentGerminationregenerationSoil compaction040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceroot system010606 plant biology & botanyWaterlogging (agriculture)Land Degradation & Development
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Management of Alluvial Forests Included in Natura 2000 91E0* Habitat Type in Maramureş Mountains Nature Park

2015

Abstract The Natura 2000 habitat type 91E0* Alluvial forests of Alnus glutinosa and Fraxinus excelsior (Alno-Padion, Alnion incanae, Salicion albae) include three subtypes of forests. In the Maramureș Mountains Nature Park (MMNP) the alluvial forests are represented by Alnus incana forest situated on the banks of mountain rivers. Starting from 2007, 70% of the MMNP is also a Natura 2000 site of community interest. In the standard form for the site are listed 18 Natura 2000 habitat types, but that of alluvial forests 91E0* is not listed either due to an error or lack of available research data. Our study seeks to provide information regarding this high conservation value habitat such as: str…

EcologyEcologyhabitat managementEcology (disciplines)sedimentsriverbanksGeographyType (biology)Habitatalluvial forestsNature parkAlluviumNatura 2000QH540-549.5Transylvanian Review of Systematical and Ecological Research
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Particularities of Grey Alder (Alnus incana) Stands in Riparian Galleries Along Streams of the Southern Transylvanian Tableland (Romania)

2019

Abstract Grey Alder (Alnus incana (L.) Moench.) stands are distributed in the Carpathian area on alluvial deposits with sediments of different grain size as galleries along rivers and streams of the sub-montane to the middle montane level. The geological structure (Tertiary sedimentary deposits) in relation to the hydromorphological processes is the base for the structure of the stream valleys, which are in part very deep. Under the special microclimate of these deeper stream stretches with lower temperatures there are favourable conditions for the development of grey alder stands.

HydrologyAlnus incanageographygeography.geographical_feature_categorybiologyEcologyMicroclimateSTREAMShabitat type 91e0biology.organism_classificationAlderGeological structuretârnava mare river basinalluvial forestssubtype alnion incanaeAlluviumSedimentary rockGeologysub-montane streamsQH540-549.5Riparian zoneTransylvanian Review of Systematical and Ecological Research
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The formation of alluvial fans and young floodplain deposits in the Lieser catchment, Eifel Mountains, western German Uplands: A study of soil erosio…

2011

This study deals with the exploration and spatiotemporal quantification of the young Holocene, nearly skeleton-free floodplain sediments of the Lieser River, a tributary of the Mosel River in the Eifel Mts. The deposits are primarily a consequence of anthropogenic-triggered soil erosion in the catchment. To observe the phenomenon of corresponding soil erosion on multiple levels two small alluvial fans of tributary catchments were investigated. For comparison, one location in the neighboring Salm valley was described. The results were compared with those of other streams. With extensive fieldwork more than 100 drillings and pits were made at 12 locations. For dating the sediments OSL dating…

HydrologyArcheologyGlobal and Planetary Changegeographygeography.geographical_feature_categoryEcologyFloodplainAlluvial fanDrainage basinPaleontologySTREAMSArchaeological artifactsTributaryOverbankHoloceneGeologyEarth-Surface ProcessesThe Holocene
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Using post-flood surveys and geomorphologic mapping to evaluate hydrological and hydraulic models: The flash flood of the Girona River (Spain) in 2007

2016

This paper analyzes the Girona River (Spain) flash flood, occurred on the 12th of October 2007, combining hydrological and hydraulic modeling with geomorphologic mapping and post-flood survey information. This research aims to reproduce the flood event in order to understand and decipher the flood processes and dynamics on a system of prograding alluvial fans. The hydrological model TETIS was used to characterize the shape and dimension of the October 2007 Girona River hydrograph. Subsequently, the flood event was reproduced using the free surface flow module of the model RiverFlow2D. The combination of hydrological and hydraulic models was evaluated using post-flood surveys defining maximu…

Hydrologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesFloodplainFlood mythHydraulic engineering0208 environmental biotechnologyFlash floodsAlluvial fanAlluvial fansGeomorphologic mappingHydrograph02 engineering and technology01 natural sciencesHydrological modeling020801 environmental engineeringPost-flood surveys100-year floodFlash floodHydraulic modelingSurface runoffGeology0105 earth and related environmental sciencesWater Science and Technology
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Late Pleistocene and Holocene landscape history of the central Palatinate forest (Pfälzerwald, south-western Germany)

2010

Abstract Field studies on the Late Pleistocene and Holocene landscape history were conducted in the central Palatinate Forest ( Pfalzerwald , Rhineland-Palatinate, Germany) near the village of Johanniskreuz. The structure and composition of periglacial cover beds, the young floodplain sediments of the Aschbach, Schwarzbach und Moosalbe valleys, and the sediment structure in some dry valleys, of alluvial fans and slope colluvia, were studied. The sandy cover beds are less than 10% aeolian, and in all cases only the main and basal layer are present, with no evidence of the intermediate layer. In general, the cover beds resemble those of other parts of the Central German Uplands ( Mittelgebirg…

Hydrologygeographygeography.geographical_feature_categoryPleistoceneAlluvial fanPreborealBorealPhysical geographyChronostratigraphyLandscape historyHoloceneGeologyEarth-Surface ProcessesSubborealQuaternary International
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