In the archaeological literature, mountains are often portrayed as the boundaries between inhabited spaces. Yet occupying high elevations may have been an adaptive choice for ancient peoples, as rapidly changing elevations also offer variation in climate and resources over a relatively small area. So what happens, instead, if we put mountain landscapes at the center of our analyses of prehistoric seasonal rounds and ecological adaptation? This Ph.D. argues that, in order to understand any landscape that includes mountains, from the Alps to the Andes, one must include the ecology and archaeology of the highest elevations. Specifically, I base my findings on new fieldwork and lithic collections from the Absaroka and Beartooth Mountains in the Greater Yellowstone Ecosystem (GYE) of the Rocky Mountains, which was a vital crossroads of prehistoric cultures for more than 11,000 years. I include five interlocking analyses. First, I consider the impacts of anthropogenic climate change on high elevation cultural resources, focusing on the diminishing resiliency of ancient high elevation ice patches and the loss of the organic artifacts and paleobiological materials they contain. Second, I create a dichotomous key for chronologically typing projectile points, suggesting a methodological improvement for typological dating in the GYE and for surface archaeology more broadly. Third, I use obsidian source data to consider whether mountain people were a single, unified group or were represented by a variety of peoples with different zones of land tenure. Fourth, I consider high elevation occupation in both mountain ranges as part of the seasonal round, using indices of diversity in tool types and raw material to study how the duration of those occupations changed through time. And, finally, I test the common contention that ancient people primarily used mountains as refugia from extreme climatic pressure at lower elevations. Ultimately, I find that, in both mountain ranges, increased high elevation activity is most highly correlated with increased population, not with hot, dry climatic conditions. In other words, the mountains were more than simply refugia for plains or basin people to occupy when pressured by climatic hardship. In addition, between the Absarokas and the Beartooths the evidence suggests two different patterns of occupation, not a monolithic pan-mountain adaptation. These results demonstrate the potential contributions of surface archaeology to our understanding of prehistory, and have important implications for the way we think about mountain landscapes as peopled spaces in relation to adjacent lower-elevation areas.

No description available.

The steep forearc slope along the northern sector of the obliquely convergent Hikurangi subduction zone is characteristic of non-accretionary and tectonically eroding continental margins, with reduced sediment supply in the trench relative to further south, and the presence of seamount relief on the Hikurangi Plateau. These seamounts influence the subduction process and the structurally-driven geomorphic development of the over-riding margin of the Australian Plate frontal wedge. The Poverty Indentation represents an unusual, especially challenging and therefore exciting location to investigate the tectonic and eustatic effects on this sedimentary system because of: (i) the geometry and obliquity of the subducting seamounts; (ii) the influence of multiple repeated seamount impacts; (iii) the effects of structurally-driven over-steeping and associated widespread occurrence of gravitational collapse and mass movements; and (iv) the development of a large canyon system down the axis of the indentation. High quality bathymetric and backscatter images of the Poverty Indentation submarine re-entrant across the northern part of the Hikurangi margin were obtained by scientists from the National Institute of Water and Atmospheric Research (NIWA) (Lewis, 2001) using a SIMRAD EM300 multibeam swath-mapping system, hull-mounted on NIWA’s research vessel Tangaroa. The entire accretionary slope of the re-entrant was mapped, at depths ranging from 100 to 3500 metres. The level of seafloor morphologic resolution is comparable with some of the most detailed Digital Elevation Maps (DEM) onshore. The detailed digital swath images are complemented by the availability of excellent high-quality processed multi-channel seismic reflection data, single channel high-resolution 3.5 kHz seismic reflection data, as well as core samples. Combined, these data support this study of the complex interactions of tectonic deformation with slope sedimentary processes and slope submarine geomorphic evolution at a convergent margin. The origin of the Poverty Indentation, on the inboard trench-slope at the transition from the northern to central sectors of the Hikurangi margin, is attributed to multiple seamount impacts over the last c. 2 Myr period. This has been accompanied by canyon incision, thrust fault propagation into the trench fill, and numerous large-scale gravitational collapse structures with multiple debris flow and avalanche deposits ranging in down-slope length from a few hundred metres to more than 40 km. The indentation is directly offshore of the Waipaoa River which is currently estimated to have a high sediment yield into the marine system. The indentation is recognised as the “Sink” for sediments derived from the Waipaoa River catchment, one of two target river systems chosen for the US National Science Foundation (NSF)-funded MARGINS “Source-to-Sink” initiative. The Poverty Canyon stretches 70 km from the continental shelf edge directly offshore from the Waipaoa to the trench floor, incising into the axis of the indentation. The sediment delivered to the margin from the Waipaoa catchment and elsewhere during sea-level high-stands, including the Holocene, has remained largely trapped in a large depocentre on the Poverty shelf, while during low-stand cycles, sediment bypassed the shelf to develop a prograding clinoform sequence out onto the upper slope. The formation of the indentation and the development of the upper branches of the Poverty Canyon system have led to the progressive removal of a substantial part of this prograding wedge by mass movements and gully incision. Sediment has also accumulated in the head of the Poverty Canyon and episodic mass flows contribute significantly to continued modification of the indentation by driving canyon incision and triggering instability in the adjacent slopes. Prograding clinoforms lying seaward of active faults beneath the shelf, and overlying a buried inactive thrust system beneath the upper slope, reveal a history of deformation accompanied by the creation of accommodation space. There is some more recent activity on shelf faults (i.e. Lachlan Fault) and at the transition into the lower margin, but reduced (~2 %) or no evidence of recent deformation for the majority of the upper to mid-slope. This is in contrast to current activity (approximately 24 to 47% shortening) across the lower slope and frontal wedge regions of the indentation. The middle to lower Poverty Canyon represents a structural transition zone within the indentation coincident with the indentation axis. The lower to mid-slope south of the canyon conforms more closely to a classic accretionary slope deformation style with a series of east-facing thrust-propagated asymmetric anticlines separated by early-stage slope basins. North of the canyon system, sediment starvation and seamount impact has resulted in frontal tectonic erosion associated with the development of an over-steepened lower to mid-slope margin, fault reactivation and structural inversion and over-printing. Evidence points to at least three main seamount subduction events within the Poverty Indentation, each with different margin responses: i) older substantial seamount impact that drove the first-order perturbation in the margin, since approximately ~1-2 Ma ii) subducted seamount(s) now beneath Pantin and Paritu Ridge complexes, initially impacting on the margin approximately ~0.5 Ma, and iii) incipient seamount subduction of the Puke Seamount at the current deformation front. The overall geometry and geomorphology of the wider indentation appears to conform to the geometry accompanying the structure observed in sandbox models after the seamount has passed completely through the deformation front. The main morphological features correlating with sandbox models include: i) the axial re-entrant down which the Poverty Canyon now incises; ii) the re-establishment of an accretionary wedge to the south of the indentation axis, accompanied by out-stepping, deformation front propagation into the trench fill sequence, particularly towards the mouth of the canyon; iii) the linear north margin of the indentation with respect to the more arcuate shape of the southern accretionary wedge; and, iv) the set of faults cutting obliquely across the deformation front near the mouth of the canyon. Many of the observed structural and geomorphic features of the Poverty Indentation also correlate well both with other sediment-rich convergent margins where seamount subduction is prevalent particularly the Nankai and Sumatra margins, and the sediment-starved Costa Rican margin. While submarine canyon systems are certainly present on other convergent margins undergoing seamount subduction there appears to be no other documented shelf to trench extending canyon system developing in the axis of such a re-entrant, as is dominating the Poverty Indentation. Ongoing modification of the Indentation appears to be driven by: i) continued smaller seamount impacts at the deformation front, and currently subducting beneath the mid-lower slope, ii) low and high sea-level stands accompanied by variations on sediment flux from the continental shelf, iii) over-steepening of the deformation front and mass movement, particularly from the shelf edge and upper slope.

Diese Dissertation befasst sich mit der Entwicklung von “Fastebenen”, die im Weiteren einheitlich als “Peneplains” bezeichnet werden, sowie dem Zerfall dieses markanten geomorphologischen Erscheinungsbildes im südlichsten Teil des tibetischen Plateau dem sogenannten Lhasa Block. Im Zuge dieser Arbeit konnten neue Erkenntnisse über die Hebungsgeschichte und der Sedimentverteilung in diesem Untersuchungsgebiet gewonnen werden. Diese Ergebnisse tragen zu einem besseren Verständnis der geodynamischen Entwicklung Asiens bei, die bis heute viele Fragen aufwirft. Ende des 19. Jahrhunderts wurden Peneplains als metastabile geomorphologische Formen angesehen, die im Zuge großflächiger Erosion entstehen. Die Bezeichnung Peneplain und das dahinter stehende Konzept werden seitdem von der geomorphologischen Gemeinschaft jedoch kontrovers diskutiert. Bis heute gibt es keine standardisierte bzw. repräsentative Definition für das nicht zu übersehende landschaftsbildende Phänomen der Peneplains. Dementsprechend gibt es auch nur wenige Ansätze zu Modellierungen oder Berechnungen mit Geoinformationssystemen. Hier, in dieser Dissertation, werden idealisierte Peneplains als erhöhte, gleichmäßige und großflächige Ebenen mit abfallenden Hängen verstanden, auch wenn sich landschaftsbildende Peneplains oft gekippt darstellen und durch tektonische Prozesse gestört bzw. bereits durch fortschreitende Erosionsprozesse angegriffen sind. Gut erhaltene Peneplains sind speziell für das Gebiet um den höchstgelegenen See der Welt, dem Nam Co, im nördlichen Teil des Lhasa Blocks im Hochland von Tibet charakteristisch. Die Peneplains zerschneiden das dort vorkommende viel ältere und vorwiegend granitische Gestein sowie die angrenzenden Metasedimente. Zur Bestimmung der Abkühl- und Hebungsalter der Granite wurden geo- und thermochronologische Methoden wie Zirkon U-Pb, Zirkon (U-Th)/He, Apatit (U-Th)/He und Apatit-SpaltspurenDatierung angewendet. Neben der Hebungsrate konnte auch die Freilegung des granitischen Gesteines ermittelt werden. Mit der Methode zur Bestimmung des U-Pb-Zirkonalters konnten zwei Intrusionsgruppen, um 118 Ma und 85 Ma, festgestellt werden. Ebenso wurden vulkanische Aktivitäten nachgewiesen und auf einen Zeitraum zwischen 63 Ma und 58 Ma datiert. Thermische Modelle, aufbauend auf Zirkon- und Apatit-(U-Th)/He-Datierungen sowie auf ApatitSpaltspuren-Daten der untersuchten Granitoide, ergeben einen Hebungs- und Abkühlungszeitraum von 75 Ma bis 55 Ma mit einer Hebungsrate von 300 m/Ma, welche im Zeitfenster zwischen 55 Ma und 45 Ma stark abfällt auf 10 m/Ma. Die Auswertung der Messdaten unserer Kooperationspartner an der Universität Münster zu kosmogenen Nukliden zeigen sehr niedrigen Erosionsraten von 6-11 m/Ma und 11-16 m/Ma, in den letzten 10.000 Jahren die in den einzelnen Einzugsgebieten ermittelt wurden. Diese Daten zeugen von einer noch immer andauernden Periode der Stabilität und tragen zur Erhaltung der Peneplains bei. Während der anhaltenden Phase der Erosion und Einebnung sind vor ungefähr 45 Ma in der untersuchten Region zwischen 3 km und 6 km Gestein abgetragen und weg transportiert worden. Es ist naheliegend, dass das abgetragene Material als Sediment über das vorhandene Flusssystem fast vollständig in die heute bestehenden Ozenane transportiert wurde. Im Lhasa Block können nur verhältnismäßig wenig Sedimente aus dieser Zeit nachgewiesen werden. Alle bisherigen Untersuchungsergebnisse sowie die durchgeführte Sediment-Herkunftsanalyse untermauern die Theorie, dass die Peneplainbildung und ihre Erosionsprozesse in niedriger Höhe - höchstwahrscheinlich auf Meeresniveau - stattgefunden haben muss. Dieser Prozess wurde durch die Kollision des indischen Kontinents mit Asien gestoppt. Die resultierende Krustenverdickung führte zu einer Hebung der Landschaft mit den Peneplains, von Meeresniveau auf 5.000 bis 7.000 Höhenmeter. Die auf dem “das Dach der Welt” vorherrschenden idealen Klimabedingungen haben anschließend für die fast vollständige Erhaltung der Peneplains gesorgt. Der zweite Teil der Dissertation befasst sich mit der Entwicklung einer robusten Methode Peneplains anhand digitale Höhenmodelle (DEM) zu berechnen bzw. zu kartieren. Frei zugängliche DEMs machen es möglich, Erdoberflächen repräsentativ mathematisch und statistisch zu analysieren und zu charakterisieren. Diese Analysemethode stellt eine ausgezeichnete Möglichkeit dar, die Peneplains mittels aussagekräftiger Algorithmen zu charakterisieren und digital zu kartieren. Um Peneplains algorithmisch von der Umgebung klar abgrenzen zu können, wurde ein komplett neuer Ansatz der Fuzzylogik angewandt. Als DEM-Basis wurde ein 90 arcsec-DEM der Shuttle Radar Topography Mission (SRTM) verwendet. Mithilfe eines Geoinformationssystems (GIS) wurden Algorithmen geschrieben, die vier verschiedene kritische Parameter zur Beschreibung von Peneplains berücksichtigen: (I) Gefälle, (II) Kurvigkeit, (III) Geländerauhigkeit und (IV) Relative Höhe. Um die Eignung der Methode zu prüfen, wurde auf Basis der SRTM-DEM weltweit kartiert und mit schon in der Literatur beschriebenen Peneplains verglichen. Die dabei erhaltenen Ergebnisse von den Appalachen, den Anden, dem Zentralmassif und Neuseeland bestätigen dass ein Einsatz des Modells, weltweit und unabhängig von der Höhenlage möglich ist.

A sustainable society is a society that satisfies its resource requirements without endangering the sustainability of these resources. The mineral endowment on the African continent is estimated to be the first or second largest of world reserves. Therefore, it is recognised that the African continent still heavily depends on mineral exports as a key contributor to the gross domestic product (GDP) of various countries. These mining activities, however, do introduce primary and secondary environmental degradation factors. They attract communities to these mining areas, light and heavy industrial establishments occur, giving rise to artisanal activities. This study focussed on satellite RS products as an aid to a mine’s operations and the monitoring of its environment. Effective operational mine management and control ensures a more sustainable and profitable lifecycle for mines. Satellite based RS holds the potential to observe the mine and its surrounding areas at high temporal intervals, different spectral wavelengths and spatial resolutions. The combination of SAR and optical information creates a spatial platform to observe and measure the mine’s operations and the behaviour of specific land cover and land use classes over time and contributes to a better understanding of the mining activities and their influence on the environment within a specific geographical area. This study will introduce an integrated methodology to collect, process and analyse spatial information over a specific targeted mine. This methodology utilises a medium resolution land cover base map, derived from Landsat 8, to understand the predominant land cover types of the surrounding area. Using very high resolution mono- and stereoscopic satellite imagery provides a finer scale analysis and identifies changes in features at a smaller scale. Combining these technologies with the synthetic aperture radar (SAR) applications for precise measurement of surface subsidence or upliftment becomes a spatial toolbox for mine management. This study examines a combination of satellite remote sensing products guided by a systematic workflow methodology to integrate spatial results as an aid for mining operations and environmental monitoring. Some of the results that can be highlighted is the successful land cover classification using the Landsat 8 satellite. The land cover that dominated the Kolomela mine area was the “SHRUBLAND/GRASS” class with a 94% coverage and “MINE” class of 2.6%. Sishen mine had a similar dominated land cover characteristic with a “SHRUBLAND/GRASS” class of 90% and “MINE” class of 4.8%. The Pléiades time-series classification analysis was done using three scenes each acquired at a different time interval. The Sishen and Kolomela mine showed especially changes from the bare soil class to the asphalt or mine class. The Pléiades stereoscopic analysis provided volumetric change detection over small, medium, large and recessed areas. Both the Sishen and Kolomela mines demonstrated height profile changes in each selected category. The last category of results focused on the SAR technology to measure within millimetre accuracy the subsidence and upliftment behaviour of surface areas over time. The Royal Bafokeng Platinum tailings pond area was measured using 74 TerraSAR-X scenes. The tailings wall area was confirmed as stable with natural subsidence that occurred in its surrounding area due to seasonal changes of the soil during rainy and dry periods. The Chuquicamata mine as a large open pit copper mine area was analysed using 52 TerraSAR-X scenes. The analysis demonstrated significant vertical surface movement over some of the dumping sites. It is the wish of the researcher that this dissertation and future research scholars will continue to contribute in this scientific field. These contributions can only assist the mining sector to continuously improve its mining operations as well as its monitoring of the primary as well as the secondary environmental impacts to ensure improved sustainability for the next generation. / Environmental Sciences / M. Sc. (Environmental Science)

Detta projekt har utförts på uppdrag av Saab Dynamics. Syftet med projektet var att skapa ett system för att ersätta den befintliga utrustning som fanns för att simulera radar vid testning av vissa vapensystem.   Systemet byggdes upp med hjälp av GPRS, GPS och transportprotokollen TCP och UDP. Huvuddelen av arbetet berörde GPS och GPRS.   Denna rapport är en redogörelse för systemets framtagning och de verktyg och metoder som användes, samt en fördjupning i ämnena GPS, GPRS och deras olika protokoll. Rapporten tar även kort upp alternativa lösningar till datasamtal.   Slutsatsen som kan dras utifrån resultatet av detta projekt är att systemet fungerar och kan vara användbart i framtiden efter vidareutveckling. / This project has been carried out on behalf of Saab Dynamics. The purpose of the project was to create a system to replace the existing equipment for simulating radar when testing certain weapon systems.   The system was created using GPRS, GPS and the transport protocols TCP and UDP. GPS and GPRS were used the most.   This report is a description of the system's design and the tools and methods used to create it, as well as an in depth look into the subjects of GPS, GPRS and their various protocols. The report also briefly discusses some alternative solutions that could have been used instead of data calls.   The conclusion that can be drawn from the results of this project is that the system works and can be useful in the future with further development.

Introdução: Prever a capacidade de resposta a fluidos continua sendo um desafio para os médicos que lidam com pacientes instáveis hemodinamicamente. A utilização de parâmetros estáticos, como pressão venosa central (PVC) tem sido usada por décadas, mas não é confiável, evidências robustas sugerem que seu uso deve ser abandonado. Ao longo dos últimos 15 anos, foram desenvolvidos vários testes dinâmicos, baseados no princípio de alteração da pré-carga cardíaca, usando as interações coração-pulmão, e, consequentemente do débito cardíaco. A elevação passiva das pernas (EPP), a infusão de pequenos volumes de fluidos, a variação da pressão de pulso (ΔPP), as variações nos diâmetros de grandes veias tem sido muito utilizados para avaliação de fluidoresponsividade (FR), neste contexto. Objetivo: Analisar e comparar medidas estáticas e dinâmicas antes, após EPP e após infusão de SF, verificando qual delas apresentam melhor FR. Métodos: Trinta e um pacientes instáveis hemodinamicamente e sob ventilação mecânica (VM) foram incluídos no estudo. Foram avaliados VTIFAO, VTIFMi, IDVCI, ΔPP, PVC, PAM antes de qualquer intervenção, após EPP e após infusão de 500ml SF. As variações dos parâmetros foram calculados para todos os pacientes. Resultados: Após EPP e infusão de SF o VTIFAO aumentou em 10% ou mais em 14 (45%) e 18 (58%) pacientes respectivamente, definidos como FR. A EPP previu a capacidade de resposta a fluidos com uma sensibilidade de 77,7%, especificidade de 100%, valor preditivo positivo de 100% e probabilidade de falso positivo de 0%. O parâmetro utilizado como padrão para FR foi o VTIFAO após SF. A PVC, o IDVCI, o ΔPP, PAM e avaliação médica não se mostraram capazes de avaliar adequadamente FR. Conclusão: Em pacientes instáveis hemodinamicamente e sob VM, a EPP foi capaz de avaliar FR com adequada sensibilidade e especificidade, podendo ser usada com segurança, antes da administração de fluidos. / Introduction: Predictig fluid responsiveness remains a constant challenge for physicians dealing with hemodynamically unstable patients. The use of static parameters, such as central venous pressure (CVP), although used for decades is not a trustworthy source, and the suggestion derived from more robust evidence suggests that the use of such should be abandoned. Over the last 15 years, various dynamic tests have been developed based on the principle of altering the cardiac preload, by using the heart-lung interactions and consequently cardiac output. Hence, Passive Leg Raising (PLR), the intake of small amounts of fluid, the variation of pulse pressure, variations in the diameter of large veins have all been widely used for evaluating fluid responsiveness (FR), within this context. Objective: The underlying objective behind this study was to test, if the non-invasive evaluation with transthoracic echocardiography, the Subaortic velocity time integral (VTI), the Distensibility Index of the Inferior Vena Cava (dIVC), the mitral velocity time integral (MTI), the (CVP) and the change in pulse pressure (ΔPP) after (PLR) and fluid infusion (500ml of saline solution) are able to predict the responsiveness of fluid therapy. Methods: Thirty one hemodynamically unstable patients, under mechanical ventilation (MV) were included in the study. Evaluations were made of VTI, MTI, DIVC), ΔPP and CVP before any intervention, after PLR and after infusion of 500ml saline solution. The variations of the parameters were calculated for all patients. Results: After PLR and infusion of saline solution, the VTI increased by 10% or more in 14 (45%) and 18 (58%) patients, respectively, defined as fluid responders. The PLR predicted a response capacity to fluids with a sensibility of 77,7%, specificity of 100%, a positive predictive value of 100% and a false positive probability of 0%. The CVP, dIVC, ΔPP, PAM and the medical evaluation were not capable of providing an adequate FR evaluation. Conclusion: In hemodynamically unstable patients under MV, PLR were capable of precisely predicting the capacity of FR. / Dissertação (Mestrado)

>Magister Scientiae - MSc

Background: ST-elevation acute myocardial infarction (STEMI) represents one of the leading causes of death. The time of STEMI onset has a circadian rhythm with a peak during diurnal hours, and the occurrence of STEMI follows a seasonal pattern with a salient peak of cases in the winter months and a marked reduction of cases in the summer months. Scholars investigated the reason behind the winter peak, suggesting that environmental and climatic factors concur in STEMI pathogenesis, but no studies have investigated whether the circadian rhythm is modified with the seasonal pattern, in particular during the summer reduction in STEMI occurrence. Methods and Results: Here, we provide a multiethnic and multination epidemiological study (from both hemispheres at different latitudes, n=2270 cases) that investigates whether the circadian variation of STEMI onset is altered in the summer season. The main finding is that the difference between numbers of diurnal (6:00 to 18:00) and nocturnal (18:00 to 6:00) STEMI is markedly decreased in the summer season, and this is a prodrome of a complex mechanism according to which the circadian rhythm of STEMI time onset seems season dependent. Conclusions: The “summer shift” of STEMI to the nocturnal interval is consistent across different populations, and the sunshine duration (a measure related to cloudiness and solar irradiance) underpins this season-dependent circadian perturbation. Vitamin D, which in our results seems correlated with this summer shift, is also primarily regulated by the sunshine duration, and future studies should investigate their joint role in the mechanisms of STEMI etiogenesis.

The aim of this thesis is to determine to what extent aircraft-borne radar remote sensing can be used as the sole method for making recordings of the surface of the earth as a basis for compiling topographical and relief maps of mountainous areas. This is done using three test areas: the Edelsberg area in the Allgäu Alps and the Silvretta and Verwall Groups in the Central Alps. The basis for discussion is provided by examination of the interaction between the objects to be imaged and the radar signal, the sensor-specific characteristics thereby being taken into account. Following this some data processing and conditioning methods used for extracting information on the relief and surface coverage for preparation of cartographical products are presented. Analysis of the quality of the results shows that, measured against the requirements of mountain cartography, radar remote sensing is a practical and useful tool for making maps in Alpine regions. As the sole source of information, however, aircraft-borne radar remote sensing p roves to date to be inadequate for cartographical applications in high-mountain regions. / Ziel der vorliegenden Arbeit ist, festzustellen, inwieweit die flugzeuggetragene Radarfernerkundung als alleinige Erfassungsmethode der Erdoberfläche zur Erstellung von topographischen und reliefbeschreibenden Karten in Gebirgslandschaften dienen kann. Dies wird anhand von drei Testgebieten, dem Edelsberggebiet in den Allgäuer Alpen sowie der Silvretta- und Verwallgrupe in den Zentralalpen, untersucht. Die Betrachtung der Interaktion zwischen den abzubildenden Objekten und dem Radar-Signal unter Berücksichtigung der sensorspezifischen Charakteristika bildet dabei die Diskussionsgrundlage. Im weiteren werden Methoden zur Datenprozessierung und -aufbereitung vorgestellt, die eine Informa-tionsextraktion bezüglich des Reliefs und der Oberflächenbedeckung für die Erstellung kartographischer Produkte ermöglichen. Die Qualitätsanalyse der Ergebnisse zeigt, dass die Radarfernerkundung, gemessen an den Anforderungen der Gebirgskartographie, ein sinnvolles und nutzbringendes Werkzeug für die Kartenerstellung in alpinen Regionen ist. Für kartographische Anwendungen in Hochgebirgsregionen erweist sich die flugzeuggetragene Radarfernerkundung als einzige Informationsquelle bislang allerdings als nicht ausreichend.