[ { "key": "PIRH6LNE", "version": 4280, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/PIRH6LNE", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/PIRH6LNE", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Kemper et al.", "parsedDate": "2024-04-25", "numChildren": 0 }, "data": { "key": "PIRH6LNE", "version": 4280, "itemType": "journalArticle", "title": "Apports de la carte géomorphologique et des matrices de Harris dans l’analyse des aménagements anthropiques : application à la grotte de La Garma (Espagne)", "creators": [ { "creatorType": "author", "firstName": "Jules", "lastName": "Kemper" }, { "creatorType": "author", "firstName": "Jean-Jacques", "lastName": "Delannoy" }, { "creatorType": "author", "firstName": "Stéphane", "lastName": "Jaillet" }, { "creatorType": "author", "firstName": "Roberto", "lastName": "Ontañon-Peredo" }, { "creatorType": "author", "firstName": "Pablo", "lastName": "Arias" } ], "abstractNote": "La découverte récente d’importants aménagements anthropiques dans des sites ornés (ex : grotte Chauvet, Nawarla Gabarnmang) ou non (ex : grotte de Bruniquel), réinterroge notre connaissance sur ces espaces souterrains et sur la manière dont ils ont été investis par les sociétés passées. La grotte de La Garma (Cantabrie, Espagne) constitue un cas d’étude exemplaire. On y relève plusieurs structures anthropiques directement associées à d’anciennes phases d’occupation et d’ornementation magdaléniennes. Cette cavité constitue de ce fait un site idéal pour développer des outils méthodologiques visant à identifier et à décomposer le palimpseste des nombreuses interventions humaines passées. L’accent est mis dans cet article sur la zone VII de la Galerie Inférieure, éloignée de près de 300 m de l’entrée paléolithique. L’utilisation conjointe de la cartographie anthropo-géomorphologique à haute résolution spatiale et des diagrammes de Harris a permis d’identifier plusieurs périodes d’aménagement de la grotte depuis le Paléolithique jusqu’à la période médiévale. La cartographie géomorphologique a permis d’identifier d’anciens aménagements parfois difficiles de lecture ; les diagrammes de Harris ont permis de décomposer dans le temps les enchaînements des gestes humains et de rendre compte de leur répartition dans la grotte. Le croisement de ces deux approches permet de reconstituer l’évolution du paysage souterrain au temps de ses fréquentations passées et de souligner ses modifications anthropiques anciennes. Cette démarche méthodologique offre un nouveau regard sur cette cavité et sur l’engagement des sociétés passées au sein d’espaces souterrains parfois éloignés des zones d’entrée.", "publicationTitle": "Géomorphologie : relief, processus, environnement", "publisher": "", "place": "", "date": "2024/04/25", "volume": "", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "", "citationKey": "", "url": "https://journals.openedition.org/geomorphologie/18109", "accessDate": "2024-04-29T16:41:36Z", "PMID": "", "PMCID": "", "ISSN": "1266-5304", "archive": "", "archiveLocation": "", "shortTitle": "Apports de la carte géomorphologique et des matrices de Harris dans l’analyse des aménagements anthropiques", "language": "fr", "libraryCatalog": "journals.openedition.org", "callNumber": "", "rights": "All rights reserved", "extra": "Publisher: Groupe français de géomorphologie", "tags": [ { "tag": "Espagne", "type": 1 }, { "tag": "Grotte", "type": 1 }, { "tag": "La Garma", "type": 1 }, { "tag": "anthropo-géomorphologie", "type": 1 }, { "tag": "archéologie", "type": 1 }, { "tag": "cartographie géomorphologique", "type": 1 }, { "tag": "diagramme de Harris", "type": 1 }, { "tag": "images 3D", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2024-04-29T16:41:36Z", "dateModified": "2024-04-29T16:41:36Z" } }, { "key": "62P5479S", "version": 4252, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/62P5479S", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/62P5479S", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "lastModifiedByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Benito-Calvo and Pérez-González", "numChildren": 0 }, "data": { "key": "62P5479S", "version": 4252, "itemType": "journalArticle", "title": "Geomorphology of the Sierra de Atapuerca and the Middle Arlanzón Valley (Burgos, Spain)", "creators": [ { "creatorType": "author", "firstName": "Alfonso", "lastName": "Benito-Calvo" }, { "creatorType": "author", "firstName": "Alfredo", "lastName": "Pérez-González" } ], "abstractNote": "The Sierra de Atapuerca is Mesozoic inlier composed of an anticlinal ridge belonging to the NW extreme of the Iberian Chain (North-Central Spain, Burgos). In this work, we present a geomorphological map of this area, developed using fieldwork, a 5 m resolution digital elevation model, aerial photographs and geological maps. The map covers 207 km2, synthesizing the geodynamic evolution of this area at 1:25,000 scale, where the geological and geomorphological characteristics of the Sierra de Atapuerca and the Middle Arlanzón Valley have facilitated the formation and preservation of archaeo-palaeoanthropological sites for over one million years. The morphogenesis of this region is determined by polygenetic landform development during the Neogene, with four planation surfaces preserved as plateaus in the landscape. During the Quaternary the incision of exoreic fluvial valleys dominated, forming a downcutting staircase model, where a sequence of 14 strath terraces dating from the Early Pleistocene developed. Other landforms in the area include landslides, cones, semi-endoreic areas, colluvial deposits and karstic landforms.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "", "volume": "0", "issue": "0", "section": "", "partNumber": "", "partTitle": "", "pages": "1-10", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2014.909339", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2014.909339", "accessDate": "2014-05-08T08:37:42Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [ "I2BAT6CT" ], "relations": { "dc:replaces": "http://zotero.org/groups/4428/items/4TXG5PPJ" }, "dateAdded": "2014-05-08T08:37:42Z", "dateModified": "2023-07-21T09:31:51Z" } }, { "key": "WZJQX6FR", "version": 4252, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/WZJQX6FR", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/WZJQX6FR", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "lastModifiedByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Serrano Giné", "numChildren": 0 }, "data": { "key": "WZJQX6FR", "version": 4252, "itemType": "journalArticle", "title": "Mapping geomorphological values from a landscape perspective", "creators": [ { "creatorType": "author", "firstName": "D.", "lastName": "Serrano Giné" } ], "abstractNote": "An easily applied methodology is developed for mapping geomorphological values from a landscape modelling perspective. The method is based on exhaustive fieldwork in which data are gathered relating to the structure and characteristics of relief, with the information weighted according to: (1) importance and significance in the area studied and (2) the viewsheds of prominent places. The procedure is applied in Muntanyes d'Ordal (Barcelona), with a large number of low-category values obtained.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "", "volume": "0", "issue": "0", "section": "", "partNumber": "", "partTitle": "", "pages": "1-9", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2014.892035", "citationKey": "", "url": "http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.892035", "accessDate": "2014-02-25T15:04:50Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [ "362FN9GJ", "I2BAT6CT" ], "relations": { "dc:replaces": "http://zotero.org/groups/4428/items/BAWIWK2R" }, "dateAdded": "2014-02-25T15:04:50Z", "dateModified": "2023-07-21T09:31:47Z" } }, { "key": "GFH2Q3IN", "version": 4237, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/GFH2Q3IN", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/GFH2Q3IN", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "lastModifiedByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Theler et al.", "parsedDate": "2010", "numChildren": 0 }, "data": { "key": "GFH2Q3IN", "version": 4237, "itemType": "journalArticle", "title": "The contribution of geomorphological mapping to sediment transfer evaluation in small alpine catchments", "creators": [ { "creatorType": "author", "firstName": "David", "lastName": "Theler" }, { "creatorType": "author", "firstName": "Emmanuel", "lastName": "Reynard" }, { "creatorType": "author", "firstName": "Christophe", "lastName": "Lambiel" }, { "creatorType": "author", "firstName": "Eric", "lastName": "Bardou" } ], "abstractNote": "The assessment of sediment transfer processes is necessary to understand the hydro-geomorphological functioning of small alpine watersheds prone to channelised debris flows because their occurrence often depends on the amount of debris available in the gully systems. Therefore, sediment budgets should be studied through the identification of erosion, transport and deposition processes. Sediment transfer processes were investigated in a small catchment by field measurements and, more specifically, through the application of a process-based geomorphological mapping method. The proposed methodology is based on data directly derived from GIS analysis using high-resolution DEM, field measurements and aerial photograph interpretations. It has been conceived to estimate sediment transfer dynamics, taking into account the role of different sediment stores in the torrential system. The proposed geomorphological mapping methodology is quite innovative in comparison with most legend systems that are not adequate for mapping comprehensively active and complex geomorphological systems such as debris flow catchments. Maps representing the various sediment storages and their relationships can be used for hydro-geomorphological hazard mitigation.", "publicationTitle": "Geomorphology", "publisher": "", "place": "", "date": "2010", "volume": "In Press, Corrected Proof", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1016/j.geomorph.2010.03.006", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/B6V93-4YKGHY6-1/2/93c14c73bb716efdfed60dc03de82387", "accessDate": "2010-03-31T11:41:02Z", "PMID": "", "PMCID": "", "ISSN": "0169-555X", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Debris flow", "type": 1 }, { "tag": "Geomorphological mapping", "type": 1 }, { "tag": "Sediment storage", "type": 1 }, { "tag": "Sediment transfer", "type": 1 }, { "tag": "Swiss Alps", "type": 1 } ], "collections": [ "I2BAT6CT", "ZQFRKKRT" ], "relations": { "dc:replaces": "http://zotero.org/groups/4428/items/E7EKPZPB" }, "dateAdded": "2010-03-31T11:41:02Z", "dateModified": "2023-07-21T09:30:16Z" } }, { "key": "2NYVVPEA", "version": 4206, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/2NYVVPEA", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/2NYVVPEA", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Siqueira et al.", "numChildren": 0 }, "data": { "key": "2NYVVPEA", "version": 4206, "itemType": "journalArticle", "title": "Evaluation of machine learning algorithms to classify and map landforms in Antarctica", "creators": [ { "creatorType": "author", "firstName": "Rafael G.", "lastName": "Siqueira" }, { "creatorType": "author", "firstName": "Gustavo V.", "lastName": "Veloso" }, { "creatorType": "author", "firstName": "Elpídio I.", "lastName": "Fernandes-Filho" }, { "creatorType": "author", "firstName": "Márcio R.", "lastName": "Francelino" }, { "creatorType": "author", "firstName": "Carlos E. G. R.", "lastName": "Schaefer" }, { "creatorType": "author", "firstName": "Guilherme R.", "lastName": "Corrêa" } ], "abstractNote": "The detailed geomorphology of ice-free landscapes of Antarctica is key to understand how their highly fragile environments respond to climate changes, at different temporal and spatial scales. Despite the recent advances in geomorphological studies of ice-free areas, machine learning applications to produce landform maps are still scarce on the Antarctic continent. In this study, we evaluated the predictive performance of different supervised machine learning algorithms to produce digital geomorphological maps in Vega Island – Antarctic Peninsula region. We tested six different models: Average Artificial Neural Networks, C5.0 Decision Tree, Random Forest, Support Vector Machine, Supervised Self Organizing Map and Weighted K-Nearest Neighbor. We used an initial set of 54 geomorphometric and spectral predictors, from which redundant variables with Pearson correlation coefficient >|0.95|were removed, and only the most important predictors for each model were selected using the Recursive Feature Elimination. For training, we ran each model 100 times and predictions were assessed by the Kappa and Global Accuracy values. The best predictors were the Red Edge 6 and SWIR 11 bands, roughness concentration index, elevation and drainage density. The decision trees C5.0 and Random Forest had the best performance, with average validation Kappa of 0.85 ± 0.03 and 0.84 ± 0.03 respectively, evidencing excellent prediction. Despite the similar performance, Random Forest showed greater uncertainty degree and accuracy when classifying complex landforms, attesting its great robustness. From sensitivity and specificity values, we observed that the glaciers and talus showed higher accuracy, whereas cryoplanated platforms and scree slopes had the worst classification. The presented methodology optimized the classification by selecting the most important predictors, assessing accuracy and evaluating uncertainty. The results indicated that machine learning methods have great potential to produce geomorphological mappings in the Antarctic ice-free areas, as a promising tool to provide detailed information on remote, harsh polar environments.", "publicationTitle": "Earth Surface Processes and Landforms", "publisher": "", "place": "", "date": "", "volume": "n/a", "issue": "n/a", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1002/esp.5253", "citationKey": "", "url": "https://onlinelibrary.wiley.com/doi/abs/10.1002/esp.5253", "accessDate": "2021-10-05T06:42:58Z", "PMID": "", "PMCID": "", "ISSN": "1096-9837", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "en", "libraryCatalog": "Wiley Online Library", "callNumber": "", "rights": "This article is protected by copyright. All rights reserved.", "extra": "_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.5253", "tags": [ { "tag": "Antarctica", "type": 1 }, { "tag": "classification", "type": 1 }, { "tag": "decision trees", "type": 1 }, { "tag": "geomorphological maps", "type": 1 }, { "tag": "geomorphometry", "type": 1 }, { "tag": "landforms", "type": 1 }, { "tag": "machine learning", "type": 1 } ], "collections": [ "I2BAT6CT", "UN94AR8C" ], "relations": { "dc:replaces": "http://zotero.org/groups/4428/items/WQKZDBT7" }, "dateAdded": "2021-10-05T06:42:58Z", "dateModified": "2023-07-21T09:22:57Z" } }, { "key": "HBK9W5HM", "version": 4148, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/HBK9W5HM", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/HBK9W5HM", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "van der Meij et al.", "parsedDate": "2021", "numChildren": 0 }, "data": { "key": "HBK9W5HM", "version": 4148, "itemType": "journalArticle", "title": "Comparing geomorphological maps made manually and by deep learning", "creators": [ { "creatorType": "author", "firstName": "W. Marijn", "lastName": "van der Meij" }, { "creatorType": "author", "firstName": "Erik W.", "lastName": "Meijles" }, { "creatorType": "author", "firstName": "Diego", "lastName": "Marcos" }, { "creatorType": "author", "firstName": "Tom T. L.", "lastName": "Harkema" }, { "creatorType": "author", "firstName": "Jasper H. J.", "lastName": "Candel" }, { "creatorType": "author", "firstName": "Gilbert J.", "lastName": "Maas" } ], "abstractNote": "Geomorphological maps provide information on the relief, genesis and shape of the earth’s surface and are widely used in sustainable spatial developments. The quality of geomorphological maps is however rarely assessed or reported, which limits their applicability. Moreover, older geomorphological maps often do not meet current quality requirements and require updating. This updating is time-consuming and because of its qualitative nature difficult to reproduce, but can be supported by novel computational methods. In this paper, we address these issues, by 1) quantifying the uncertainty associated with manual geomorphological mapping, 2) exploring the use of Convolutional Neural Networks (CNNs) for semi-automated geomorphological mapping, and 3) testing the sensitivity of CNNs to uncertainties in manually created evaluation data. We selected a test area in the Dutch push-moraine district with a pronounced relief and a high variety of landforms. For this test area we developed five manually created geomorphological maps and 27 automatically created landform maps using CNNs. The resulting manual maps are similar on a regional level. We could identify the causes of disagreement between the maps on a local level, which often related to differences in mapping experience, choices in delineation and different interpretations of the legend. Coordination of mapping efforts and field validation are necessary to create accurate and precise maps. CNNs perform well in identifying landforms and geomorphological units, but fail at correct delineation. The human geomorphologist remains necessary to correct the delineation and classification of the computed maps. The uncertainty in the manually created data that are used to train and evaluate CNNs have a large effect on the model performance and evaluation. This also advocates for coordinated mapping efforts to ensure the quality of manually created training and test data. Further model development and data processing are required before CNNs can act as standalone mapping techniques.", "publicationTitle": "Earth Surface Processes and Landforms", "publisher": "", "place": "", "date": "2021", "volume": "n/a", "issue": "n/a", "section": "", "partNumber": "", "partTitle": "", "pages": "", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1002/esp.5305", "citationKey": "", "url": "https://onlinelibrary.wiley.com/doi/abs/10.1002/esp.5305", "accessDate": "2021-12-21T11:13:12Z", "PMID": "", "PMCID": "", "ISSN": "1096-9837", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "en", "libraryCatalog": "Wiley Online Library", "callNumber": "", "rights": "", "extra": "_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.5305", "tags": [ { "tag": "The Netherlands", "type": 1 }, { "tag": "convolutional neural network", "type": 1 }, { "tag": "deep learning", "type": 1 }, { "tag": "geomorphological map", "type": 1 }, { "tag": "geomorphology", "type": 1 }, { "tag": "mapping", "type": 1 }, { "tag": "uncertainty", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2021-12-21T11:13:12Z", "dateModified": "2021-12-21T11:13:22Z" } }, { "key": "V9VUKF49", "version": 4144, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/V9VUKF49", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/V9VUKF49", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "lastModifiedByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Annys et al.", "numChildren": 0 }, "data": { "key": "V9VUKF49", "version": 4144, "itemType": "journalArticle", "title": "Geomorphology of the Durmitor Mountains and surrounding plateau Jezerska Površ (Montenegro)", "creators": [ { "creatorType": "author", "firstName": "Klaas", "lastName": "Annys" }, { "creatorType": "author", "firstName": "Amaury", "lastName": "Frankl" }, { "creatorType": "author", "firstName": "Velibor", "lastName": "Spalević" }, { "creatorType": "author", "firstName": "Milic", "lastName": "Čurović" }, { "creatorType": "author", "firstName": "Dragan", "lastName": "Borota" }, { "creatorType": "author", "firstName": "Jan", "lastName": "Nyssen" } ], "abstractNote": "The geomorphological map of the northeastern Durmitor Mountains and the plateau Jezerska Površ (1:10,000, 47 km², Montenegro, Dinaric Alps) was prepared from an intensive fieldwork campaign and remote sensing analysis, and was compiled within a GIS. The basic components of the legend are (i) processes/genesis, (ii) materials, (iii) morphometry/morphography, (iv) hydrography, (v) vegetation and (vi) anthropogenic features. The geomorphological setting of the area consists of Mesozoic limestones which are physically deformed by Quaternary glacial and periglacial activity and chemically affected during interglacials. Glacial deposits on the plateau of three middle-to-late Pleistocene glacial phases are intersected by a well-developed network of palaeo meltwater channels. In the mountains, Holocene glacier retreat left behind a series of well-preserved recessional moraines. The map serves as a valuable tool for Quaternary research in the Durmitor Mountains, and also in other mountains of the Western Balkans.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "", "volume": "10", "issue": "4", "section": "", "partNumber": "", "partTitle": "", "pages": "1-12", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2014.909338", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2014.909338", "accessDate": "2014-05-08T08:37:52Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [], "collections": [ "I2BAT6CT" ], "relations": { "dc:replaces": "http://zotero.org/groups/4428/items/DDFGBCX7" }, "dateAdded": "2014-05-08T08:37:52Z", "dateModified": "2021-11-12T13:58:53Z" } }, { "key": "HP89WA3Z", "version": 3987, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/HP89WA3Z", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/HP89WA3Z", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Quesada-Román and Pérez-Briceño", "parsedDate": "2019-07-03", "numChildren": 0 }, "data": { "key": "HP89WA3Z", "version": 3987, "itemType": "journalArticle", "title": "Geomorphology of the Caribbean coast of Costa Rica", "creators": [ { "creatorType": "author", "firstName": "Adolfo", "lastName": "Quesada-Román" }, { "creatorType": "author", "firstName": "Paula M.", "lastName": "Pérez-Briceño" } ], "abstractNote": "Costa Rica’s Caribbean coastline is the result of a complex tectonic setting coupled with dynamic geological, climatological, hydrological and ecological processes. Despite their importance in risk prevention and in land use planning, geomorphological maps at detailed scales are scarce in Costa Rica. A geomorphology map of 210 km of the Caribbean coastline was produced at a scale of 1: 25,000 with a 1: 50,000 scale output map. Eleven landforms were mapped and described based upon their morphogenesis (i.e. tectonic, volcanic, fluvial and/or coastal). This work is an important base for coastal management, and is a compilation of the best existing knowledge of the Caribbean coast of Costa Rica.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "July 3, 2019", "volume": "15", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "363-371", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2019.1600592", "citationKey": "", "url": "https://doi.org/10.1080/17445647.2019.1600592", "accessDate": "2019-07-18T15:48:26Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Caribbean Sea", "type": 1 }, { "tag": "Central America", "type": 1 }, { "tag": "Geomorphological mapping", "type": 1 }, { "tag": "coastal geomorphology", "type": 1 }, { "tag": "coastal management", "type": 1 }, { "tag": "fluvial geomorphology", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2019-07-18T15:48:26Z", "dateModified": "2019-07-18T15:48:26Z" } }, { "key": "E3E59TRU", "version": 3987, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/E3E59TRU", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/E3E59TRU", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Walk et al.", "parsedDate": "2019-07-03", "numChildren": 0 }, "data": { "key": "E3E59TRU", "version": 3987, "itemType": "journalArticle", "title": "Geomorphology of the coastal alluvial fan complex Guanillos, northern Chile", "creators": [ { "creatorType": "author", "firstName": "Janek", "lastName": "Walk" }, { "creatorType": "author", "firstName": "Georg", "lastName": "Stauch" }, { "creatorType": "author", "firstName": "Melanie", "lastName": "Bartz" }, { "creatorType": "author", "firstName": "Helmut", "lastName": "Brückner" }, { "creatorType": "author", "firstName": "Frank", "lastName": "Lehmkuhl" } ], "abstractNote": "The evolution of alluvial fans on the narrow coastal plain of the Atacama Desert in northern Chile is so far poorly investigated. Therefore, a detailed geomorphological map at a scale of 1:7500 of a coastal alluvial fan complex at Guanillos (21°58′S, 70°10.5′W) is provided as a first step to understand the fan’s morphogenesis. Geomorphological mapping was based on a digital elevation model with a resolution of 2 m generated from Pleiades-1 tri-stereo satellite imagery, derived terrain parameters, and on-site field mapping. The resultant map is used to characterize and categorize the overall morphology of the alluvial fan complex. In particular, linear features constructed by primary alluvial fan processes can be differentiated successfully from those developed by secondary processes. Furthermore, the advanced evolutionary state of the fan complex is revealed. We introduce a morphostratigraphic model comprising the fan’s prograde evolution, dissection, and successive abandonment of surface generations.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "July 3, 2019", "volume": "15", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "436-447", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2019.1611499", "citationKey": "", "url": "https://doi.org/10.1080/17445647.2019.1611499", "accessDate": "2019-07-18T15:48:02Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Atacama Desert", "type": 1 }, { "tag": "Geomorphological map", "type": 1 }, { "tag": "Pleiades", "type": 1 }, { "tag": "alluvial fan", "type": 1 }, { "tag": "coastal Cordillera", "type": 1 }, { "tag": "northern Chile", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2019-07-18T15:48:02Z", "dateModified": "2019-07-18T15:48:02Z" } }, { "key": "GVX4IWLH", "version": 3987, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/GVX4IWLH", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/GVX4IWLH", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Tsanakas et al.", "parsedDate": "2019-07-03", "numChildren": 0 }, "data": { "key": "GVX4IWLH", "version": 3987, "itemType": "journalArticle", "title": "Geomorphology of the Pieria Mtns, Northern Greece", "creators": [ { "creatorType": "author", "firstName": "K.", "lastName": "Tsanakas" }, { "creatorType": "author", "firstName": "E.", "lastName": "Karymbalis" }, { "creatorType": "author", "firstName": "K.", "lastName": "Gaki-Papanastassiou" }, { "creatorType": "author", "firstName": "H.", "lastName": "Maroukian" } ], "abstractNote": "The present study is an attempt to comprehend and interpret the geomorphological factors that contributed to the landscape formation and evolution of the broader area of Pieria Mtns in Northern Greece. Detailed geomorphological mapping was performed utilizing both automated - GIS oriented and traditional geomorphological techniques. In order to scientifically determine the formation and evolution of present day landscape, topography, geology, tectonics and climatic status were taken into consideration. The broader area of Pieria Mtns is a landscape with heterogeneous geomorphological environments. The geomorphological formation and evolution is the result of primarily active tectonics, and exogenic processes from Lower Miocene until present. The combined methodology of GIS oriented and traditional geomorphological mapping was proved to be scientifically accurate although time consuming. Detailed field work was considered mandatory in order to validate the GIS derivatives, and interpret the genesis of the landforms.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "July 3, 2019", "volume": "15", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "499-508", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2019.1619630", "citationKey": "", "url": "https://doi.org/10.1080/17445647.2019.1619630", "accessDate": "2019-07-18T15:47:41Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Geomorphology", "type": 1 }, { "tag": "Katerini", "type": 1 }, { "tag": "Northern Greece", "type": 1 }, { "tag": "Pieria Mtns", "type": 1 }, { "tag": "geomorphological mapping", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2019-07-18T15:47:41Z", "dateModified": "2019-07-18T15:47:41Z" } }, { "key": "F7NV9BEL", "version": 3987, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/F7NV9BEL", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/F7NV9BEL", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Quesada-Román et al.", "parsedDate": "2019-07-03", "numChildren": 0 }, "data": { "key": "F7NV9BEL", "version": 3987, "itemType": "journalArticle", "title": "Glacial geomorphology of the Chirripó National Park, Costa Rica", "creators": [ { "creatorType": "author", "firstName": "Adolfo", "lastName": "Quesada-Román" }, { "creatorType": "author", "firstName": "Juan Antonio", "lastName": "Ballesteros-Cánovas" }, { "creatorType": "author", "firstName": "Markus", "lastName": "Stoffel" }, { "creatorType": "author", "firstName": "José Juan", "lastName": "Zamorano-Orozco" } ], "abstractNote": "Several regions of tropical America show imprints of past glacial activity. These relict landforms can support the understanding of past climate conditions, such as during the Last Glacial Maximum (LGM), and the implications that these paleoclimatic conditions could have had on landscape change. Here, we present and analyze glacial morphologies for the Chirripó National Park in Costa Rica based on aerial imagery (1:25,000), detailed Digital Elevation Models, geomorphic mapping, as well as geomorphic assessments in the field to determine and validate landforms. This study adds valuable insights into the reconstruction of the maximum expansion of tropical glaciation during the LGM in Costa Rica and into tropical America glacial landscapes in general.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "July 3, 2019", "volume": "15", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "538-545", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2019.1625822", "citationKey": "", "url": "https://doi.org/10.1080/17445647.2019.1625822", "accessDate": "2019-07-18T15:47:21Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Central America", "type": 1 }, { "tag": "Geomorphological mapping", "type": 1 }, { "tag": "Last Glacial Maximum", "type": 1 }, { "tag": "glaciation", "type": 1 }, { "tag": "late Quaternary", "type": 1 }, { "tag": "tropical mountains", "type": 1 }, { "tag": "tropics", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2019-07-18T15:47:21Z", "dateModified": "2019-07-18T15:47:21Z" } }, { "key": "CK5SK8WY", "version": 3987, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/CK5SK8WY", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/CK5SK8WY", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Coratza et al.", "parsedDate": "2019-07-03", "numChildren": 0 }, "data": { "key": "CK5SK8WY", "version": 3987, "itemType": "journalArticle", "title": "Geomorphology of the Rio Cisles basin (Odle Group, Dolomites, Italy)", "creators": [ { "creatorType": "author", "firstName": "Paola", "lastName": "Coratza" }, { "creatorType": "author", "firstName": "Alessandro", "lastName": "Ghinoi" }, { "creatorType": "author", "firstName": "Mauro", "lastName": "Marchetti" }, { "creatorType": "author", "firstName": "Mauro", "lastName": "Soldati" } ], "abstractNote": "The results of geomorphological investigations carried out in the Rio Cisles basin in the Odle Group (Italian Alps) are presented. This is one of the most famous and spectacular mountain groups of the Dolomites, located in the north-western sector of the Gardena valley, an area of high tourism appeal. Field surveys and multitemporal aerial-photo interpretation led to the production of a geomorphological map at a 1:12,000 scale. This map outlines the features of an area of about 20 km2, characterised by high relief energy, mainly due to the overlapping of large dolomite rocks masses on clayey rocks. The present morphology is the result of intense postglacial and paraglacial geomorphic activity, which has affected the area since the Upper Pleistocene. The geomorphological evolution of this area has been reconstructed and a new contribution is given to the comprehension of the geomorphology of the eastern Dolomites.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "July 3, 2019", "volume": "15", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "546-554", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2019.1633426", "citationKey": "", "url": "https://doi.org/10.1080/17445647.2019.1633426", "accessDate": "2019-07-18T15:47:07Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Dolomites", "type": 1 }, { "tag": "Gardena valley", "type": 1 }, { "tag": "High-mountain", "type": 1 }, { "tag": "Italy", "type": 1 }, { "tag": "geomorphological mapping", "type": 1 }, { "tag": "mountain geomorphology", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2019-07-18T15:47:07Z", "dateModified": "2019-07-18T15:47:07Z" } }, { "key": "LQK7L9MP", "version": 3867, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/LQK7L9MP", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/LQK7L9MP", "type": "text/html" } }, "meta": { "createdByUser": { "id": 1221415, "username": "CedocIGD", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigd", "type": "text/html" } } }, "creatorSummary": "Lastochkin et al.", "parsedDate": "2018-02-15", "numChildren": 0 }, "data": { "key": "LQK7L9MP", "version": 3867, "itemType": "journalArticle", "title": "System-morphological approach: Another look at morphology research and geomorphological mapping", "creators": [ { "creatorType": "author", "firstName": "Alexander N.", "lastName": "Lastochkin" }, { "creatorType": "author", "firstName": "Andrey I.", "lastName": "Zhirov" }, { "creatorType": "author", "firstName": "Sergei F.", "lastName": "Boltramovich" } ], "abstractNote": "A large number of studies require a clear and unambiguous morphological basis. For over thirty years, Russian scientists have been applying a system-morphological approach for the Arctic and Antarctic research, ocean floor investigation, for various infrastructure construction projects (oil and gas, sports, etc.), in landscape and environmental studies. This article is a review aimed to introduce this methodological approach to the international scientific community. The details of the methods and techniques can be found in a series of earlier papers published in the Russian language in 1987–2016. The proposed system-morphological approach includes: 1) partitioning of the Earth surface, i.e. precise identification of linear, point, and areal elements of topography considered as a two-dimensional surface without any geological substance; 2) further identification of larger formations: geomorphological systems and regions; 3) analysis of structural relations and symmetry of topography; and 4) various dynamic (litho- and glaciodynamic, tectonic, etc.) interpretations of the observed morphology. This method can be used to study the morphology of the surface topography as well as less accessible interfaces such as submarine and subglacial ones.", "publicationTitle": "Geomorphology", "publisher": "", "place": "", "date": "February 15, 2018", "volume": "303", "issue": "", "section": "", "partNumber": "", "partTitle": "", "pages": "486-503", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "Geomorphology", "DOI": "10.1016/j.geomorph.2017.10.022", "citationKey": "", "url": "http://www.sciencedirect.com/science/article/pii/S0169555X16310352", "accessDate": "2018-02-14T13:18:33Z", "PMID": "", "PMCID": "", "ISSN": "0169-555X", "archive": "", "archiveLocation": "", "shortTitle": "System-morphological approach", "language": "", "libraryCatalog": "ScienceDirect", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Geomorphological mapping", "type": 1 }, { "tag": "Geomorphology", "type": 1 }, { "tag": "Morphology research", "type": 1 }, { "tag": "System-morphological approach", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2018-02-14T13:18:33Z", "dateModified": "2018-02-14T13:18:33Z" } }, { "key": "PGXNNJ6T", "version": 3820, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/PGXNNJ6T", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/PGXNNJ6T", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Miklín and Galia", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "PGXNNJ6T", "version": 3820, "itemType": "journalArticle", "title": "Detailed fluvial-geomorphologic mapping of wadeable streams: a proposal of universal map symbology", "creators": [ { "creatorType": "author", "firstName": "Jan", "lastName": "Miklín" }, { "creatorType": "author", "firstName": "Tomáš", "lastName": "Galia" } ], "abstractNote": "Detailed maps are important components of fluvial-geomorphological research, connecting several tools, namely field mapping of presented channel and floodplain forms and the assessment of fluvial processes and hydromorphological conditions of current river management. In this paper, we propose a universal map legend for the complex mapping of small stream channels in a detailed scale, which means including both the channel and adjacent floodplain segments. With the help of the symbology we are able to demonstrate both fluvial forms (i.e. individual features, grain size of bed sediments and fluvial deposits) and fluvial processes (i.e. contemporary trends in channels, character of lateral sediment inputs and flow characteristics) in a single map. In total, nearly 150 symbols were proposed and created as a combination of TrueType font and ArcGIS Style files. However, the principle can be used in various software. The work is accompanied by three map examples from the Nízký Jeseník Mts (the Stará Voda Stream) and the Moravskoslezské Beskydy Mts (the Lubina and Bystrý Streams).", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "November 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "698-706", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1355275", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1355275", "accessDate": "2017-09-19T14:16:42Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "Detailed fluvial-geomorphologic mapping of wadeable streams", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "ESRI ArcGIS", "type": 1 }, { "tag": "Fluvial geomorphology", "type": 1 }, { "tag": "Map symbols", "type": 1 }, { "tag": "high-gradient streams", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-09-19T14:16:42Z", "dateModified": "2017-09-19T14:16:42Z" } }, { "key": "CAK2UHMA", "version": 3817, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/CAK2UHMA", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/CAK2UHMA", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Bendle et al.", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "CAK2UHMA", "version": 3817, "itemType": "journalArticle", "title": "The glacial geomorphology of the Lago Buenos Aires and Lago Pueyrredón ice lobes of central Patagonia", "creators": [ { "creatorType": "author", "firstName": "Jacob M.", "lastName": "Bendle" }, { "creatorType": "author", "firstName": "Varyl R.", "lastName": "Thorndycraft" }, { "creatorType": "author", "firstName": "Adrian P.", "lastName": "Palmer" } ], "abstractNote": "This paper presents a glacial geomorphological map of landforms produced by the Lago General Carrera–Buenos Aires and Lago Cochrane–Pueyrredón ice lobes of the former Patagonian Ice Sheet. Over 35,000 landforms were digitized into a Geographical Information System from high-resolution (<15 m) satellite imagery, supported by field mapping. The map illustrates a rich suite of ice-marginal glacigenic, subglacial, glaciofluvial and glaciolacustrine landforms, many of which have not been mapped previously (e.g. hummocky terrain, till eskers, eskers). The map reveals two principal landform assemblages in the central Patagonian landscape: (i) an assemblage of nested latero-frontal moraine arcs, outwash plains or corridors, and inset hummocky terrain, till eskers and eskers, which formed when major ice lobes occupied positions on the Argentine steppe; and (ii) a lake-terminating system, dominated by the formation of glaciolacustrine landforms (deltas, shorelines) and localized ice-contact glaciofluvial features (e.g. outwash fans), which prevailed during deglaciation.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "November 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "654-673", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1351908", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1351908", "accessDate": "2017-07-27T14:13:32Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Glacial geomorphology", "type": 1 }, { "tag": "Patagonia", "type": 1 }, { "tag": "Patagonian Ice Sheet", "type": 1 }, { "tag": "ice lobes", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-07-27T14:13:32Z", "dateModified": "2017-07-27T14:13:32Z" } }, { "key": "7CDEJAT6", "version": 3813, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/7CDEJAT6", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/7CDEJAT6", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Martinez-Graña et al.", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "7CDEJAT6", "version": 3813, "itemType": "journalArticle", "title": "Geomorphology of the mouth of the Arosa estuary (Coruña-Pontevedra, Spain)", "creators": [ { "creatorType": "author", "firstName": "A. M.", "lastName": "Martinez-Graña" }, { "creatorType": "author", "firstName": "L.", "lastName": "Arias" }, { "creatorType": "author", "firstName": "J. L.", "lastName": "Goy" }, { "creatorType": "author", "firstName": "C.", "lastName": "Zazo" }, { "creatorType": "author", "firstName": "P.", "lastName": "Silva" } ], "abstractNote": "This paper presents a geomorphological analysis of the littoral zone of the Arosa-Pontevedra estuary mouth and identifies geomorphological units and categorizes them into morphogenetic systems. The different morphogenetic systems are used to establish a comprehensive evolutionary analysis, contrasting the depositional systems found in the continental littoral zone with the marine erosional systems (‘rasas’). The compiled cartography groups the geomorphological units into the following: the lithoestructural morphogenetic system with large-scale forms (domes, inselbergs, residual relief, etc.) and small-scale forms (gnammas, tafoni, channels, etc.); the littoral morphogenetic system comprised of marine (marine terraces, beaches, tidal bars, tombolos and coastal arrows), transition (marshes, lagoons and fan deltas) and eolian (dune systems) settings; the fluvial morphogenetic system with channelled (alluvial, flood plain and river terraces), transition (alluvial fans and alluvial cones) and sheet flood (pediments and glacis) systems; the gravitational morphogenetic system (colluvium); and the alteration morphogenetic system (sand-alteration).", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "November 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "554-562", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1340198", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1340198", "accessDate": "2017-07-17T15:39:08Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Galicia", "type": 1 }, { "tag": "Geomorphological map", "type": 1 }, { "tag": "NW Spain", "type": 1 }, { "tag": "morphogenetic systems", "type": 1 }, { "tag": "the rosa estuary", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-07-17T15:39:08Z", "dateModified": "2017-07-17T15:39:08Z" } }, { "key": "U4I38K3F", "version": 3813, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/U4I38K3F", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/U4I38K3F", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Norris et al.", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "U4I38K3F", "version": 3813, "itemType": "journalArticle", "title": "Glacial landforms of northwest Saskatchewan", "creators": [ { "creatorType": "author", "firstName": "Sophie L.", "lastName": "Norris" }, { "creatorType": "author", "firstName": "Martin", "lastName": "Margold" }, { "creatorType": "author", "firstName": "Duane G.", "lastName": "Froese" } ], "abstractNote": "A comprehensive map of glacial landforms is presented for the area of northwest Saskatchewan, Canada. Remote sensing of 1-arc (∼30 m resolution) Shuttle Radar Topography Mission digital elevation models over an area of approximately 15,000 km2 were used as the primary data source for landform identification. A total of 16,856 landforms were identified pertaining to Quaternary glacial and postglacial activity. Ten landform types were mapped: ice flow parallel lineations (flutings, drumlins, mega-scale glacial lineations, and crag-and-tail ridges), moraines (major and minor), ice-thrust ridges, crevasse-fill ridges, meltwater landforms (major and minor meltwater channels and eskers), palaeo-shorelines and dunes. Collectively, these landforms constitute a glacial and postglacial landform record, which exhibits a more complex pattern than previously recognised, with evidence of multiple cross cutting ice flow directions. This geomorphological mapping of the regional landform record provides the prerequisite for future reconstructions of the glacial dynamics and chronology of northwest Saskatchewan.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "November 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "600-607", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1342212", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1342212", "accessDate": "2017-07-17T15:38:46Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Glacial geomorphology", "type": 1 }, { "tag": "Laurentide ice sheet", "type": 1 }, { "tag": "northwest Saskatchewan", "type": 1 }, { "tag": "palaeoglaciology", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-07-17T15:38:46Z", "dateModified": "2017-07-17T15:38:46Z" } }, { "key": "Z9STNGUM", "version": 3813, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/Z9STNGUM", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/Z9STNGUM", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Peterson et al.", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "Z9STNGUM", "version": 3813, "itemType": "journalArticle", "title": "Glacial geomorphology of the south Swedish uplands – focus on the spatial distribution of hummock tracts", "creators": [ { "creatorType": "author", "firstName": "Gustaf", "lastName": "Peterson" }, { "creatorType": "author", "firstName": "Mark D.", "lastName": "Johnson" }, { "creatorType": "author", "firstName": "Colby A.", "lastName": "Smith" } ], "abstractNote": "We present the first comprehensive glacial-landform map of the south Swedish uplands (SSU), deglaciated 15–13 ka ago, using one consistent method and dataset; a Light Detection and Ranging-derived digital elevation model. In particular, this map focuses on the spatial distribution of hummock tracts. The distribution of hummock tracts reinforces previous thinking of a broad lobate east–west zone of hummocks across the southern part of the SSU. But this map also reveals a pattern of hummock tracts confined in what we call hummock corridors that have a radial pattern sub-parallel to the overall ice-flow direction. Hummocks occur in a wide variety of morphologies, but we also show the distribution of two distinct forms: V-shaped hummocks and ‘ribbed moraine’. Cross-cutting relationships between hummocks and glacial lineations indicate a more complex chronology than previously suggested. In places, lineations are overlain by hummocks and in other places hummocks are overlain by lineations. Additionally, directional variation of glacial lineations together with a complex end-moraine pattern suggests a dynamic ice sheet with multiple small lobes. Finally, mapped end moraines help to better correlate the deglacial timescales of western and eastern Sweden.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "November 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "534-544", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1336121", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1336121", "accessDate": "2017-07-17T15:38:16Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Glacial geomorphology", "type": 1 }, { "tag": "deglaciation", "type": 1 }, { "tag": "hummocks", "type": 1 }, { "tag": "paleo-glaciology", "type": 1 }, { "tag": "southern Sweden", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-07-17T15:38:16Z", "dateModified": "2017-07-17T15:38:16Z" } }, { "key": "XEQ5GCM8", "version": 3796, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/XEQ5GCM8", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/XEQ5GCM8", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Borsellino et al.", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "XEQ5GCM8", "version": 3796, "itemType": "journalArticle", "title": "Glacial geomorphology of the Barbizon & Butler Downs, Rangitata Valley, South Island, New Zealand", "creators": [ { "creatorType": "author", "firstName": "Rosabella", "lastName": "Borsellino" }, { "creatorType": "author", "firstName": "James", "lastName": "Shulmeister" }, { "creatorType": "author", "firstName": "Stefan", "lastName": "Winkler" } ], "abstractNote": "The inland valleys of New Zealand’s South Island were heavily glaciated during the last glacial cycle. Subsequent fluvial incision has eroded out glacial deposits from the valleys in many locations, making it difficult to reconstruct glacial dynamics and chronology. The Brabazon and Butler Downs lie in a fault-controlled intra-montaine basin that has been largely protected from fluvial erosion and the area contains extensive evidence for multiple glacial margins. This paper presents a detailed glacial geomorphology map of the Brabazon and Butler Downs at a scale of 1:20,000. Glacial landforms have been mapped and subdivided into three main zones: an upper zone distinguished by a flight of kame terraces, a middle zone containing kettles and meltwater channels, and a lower zone of lateral moraines. The new map provides insight into former glacial environments in the region and provides a related framework for future paleoclimate reconstructions.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "November 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "502-510", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1336122", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1336122", "accessDate": "2017-06-21T14:07:46Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Glacial geomorphology", "type": 1 }, { "tag": "Moraines", "type": 1 }, { "tag": "New Zealand", "type": 1 }, { "tag": "Rangitata", "type": 1 }, { "tag": "kame terraces", "type": 1 }, { "tag": "kettles", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-06-21T14:07:46Z", "dateModified": "2017-06-21T14:07:46Z" } }, { "key": "MRZ45RKF", "version": 3796, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/MRZ45RKF", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/MRZ45RKF", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Buosi et al.", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "MRZ45RKF", "version": 3796, "itemType": "journalArticle", "title": "Geomorphology and sedimentology of Porto Pino, SW Sardinia, western Mediterranean", "creators": [ { "creatorType": "author", "firstName": "Carla", "lastName": "Buosi" }, { "creatorType": "author", "firstName": "Sira", "lastName": "Tecchiato" }, { "creatorType": "author", "firstName": "Nicola", "lastName": "Pusceddu" }, { "creatorType": "author", "firstName": "Paolo", "lastName": "Frongia" }, { "creatorType": "author", "firstName": "Angelo", "lastName": "Ibba" }, { "creatorType": "author", "firstName": "Sandro De", "lastName": "Muro" } ], "abstractNote": "This paper presents a detailed (1:4000) geomorphological, sedimentological and ecological map of a Mediterranean microtidal wave-dominated beach system and adjacent inner shelf. This map is an innovative cartographic product that integrates a range of processes of present and past timeframes. It is part of a larger cartography on the coastal geomorphology of Sardinia (Italy) aiming to facilitate coastal management practices and future scientific research. The study area is located in SW Sardinia (Italy), and focuses on Porto Pino beach, an important tourist destination of semi-pristine nature, facing environmental pressures common to many coastal Mediterranean settings. In this context, the main human impact on coastal dune habitats is described and a full environmental characterization of the beach system is presented.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "November 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "470-485", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1328318", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1328318", "accessDate": "2017-06-21T14:07:26Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Mediterranean Sea", "type": 1 }, { "tag": "Posidonia oceanica meadow; beach management", "type": 1 }, { "tag": "Sedimentology", "type": 1 }, { "tag": "coastal geomorphology", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-06-21T14:07:26Z", "dateModified": "2017-06-21T14:07:26Z" } }, { "key": "HJZ3VMNP", "version": 3795, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/HJZ3VMNP", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/HJZ3VMNP", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Prampolini et al.", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "HJZ3VMNP", "version": 3795, "itemType": "journalArticle", "title": "Geomorphological mapping of terrestrial and marine areas, northern Malta and Comino (central Mediterranean Sea)", "creators": [ { "creatorType": "author", "firstName": "Mariacristina", "lastName": "Prampolini" }, { "creatorType": "author", "firstName": "Federica", "lastName": "Foglini" }, { "creatorType": "author", "firstName": "Sara", "lastName": "Biolchi" }, { "creatorType": "author", "firstName": "Stefano", "lastName": "Devoto" }, { "creatorType": "author", "firstName": "Serafino", "lastName": "Angelini" }, { "creatorType": "author", "firstName": "Mauro", "lastName": "Soldati" } ], "abstractNote": "This paper presents an integrated geomorphological map of terrestrial and marine areas of northern Malta and Comino (central Mediterranean Sea) at 1:25,000 scale. The map is the result of terrestrial and marine analyses of different types of data such as aerial photos, digital terrain model of the seafloor and its acoustic backscatter image. The research is intended to emphasise the relationships and continuity of geomorphological features of both the land- and sea-scape, and outline their evolution. The map highlights the occurrence of fluvial, karst and gravity-induced landforms both on land and on the seafloor, such as palaeo-fluvial channels, sinkholes and landslides, which were shaped during sea level lowstands of the last glacial cycle.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "November 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "457-469", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1327507", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1327507", "accessDate": "2017-06-21T14:07:06Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Geomorphological mapping", "type": 1 }, { "tag": "Landslides", "type": 1 }, { "tag": "Malta", "type": 1 }, { "tag": "coastal geomorphology", "type": 1 }, { "tag": "submarine geomorphology", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-06-21T14:07:06Z", "dateModified": "2017-06-21T14:07:06Z" } }, { "key": "2FSR2HQK", "version": 3791, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/2FSR2HQK", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/2FSR2HQK", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "González-Gutiérrez et al.", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "2FSR2HQK", "version": 3791, "itemType": "journalArticle", "title": "Geomorphology of the Curueño River headwaters, Cantabrian mountains (NW Spain)", "creators": [ { "creatorType": "author", "firstName": "R. B.", "lastName": "González-Gutiérrez" }, { "creatorType": "author", "firstName": "J.", "lastName": "Santos-González" }, { "creatorType": "author", "firstName": "A.", "lastName": "Gómez-Villar" }, { "creatorType": "author", "firstName": "J. M.", "lastName": "Redondo-Vega" }, { "creatorType": "author", "firstName": "I.", "lastName": "Prieto-Sarro" } ], "abstractNote": "The article presents the 1:25,000-scale geomorphological map of the upper reaches of the Curueño River, on the southern slope of the Central Cantabrian Mountains, NW Spain. The study area spans approximately 125 km2 and corresponds to the 1:25,000-scale Spanish National Topographical Map Sheet 104-I of Lugueros. The area is moderately mountainous with elevation ranging from 1100 to 2100 m.a.s.l. The main landforms are river gorges, karst, and glacial landforms. The map legend contains 78 elements divided into 9 groups: litho-structural, polygenic, karst, fluvial, glacial, periglacial, nival, gravitational, weathering, and anthropic forms. The map was prepared using Esri ArcGIS with the Universal Transverse Mercator (UTM, Zone 30) projection. In addition, a database and style set were created for each landform with the goal of using this set of symbols in other areas and performing complementary mapping of geologic and geomorphologic risk, protection of natural geoheritage, land-use classification, and applied geomorphology.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "novembre 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "382-394", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1316217", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1316217", "accessDate": "2017-05-12T15:09:12Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Cantabrian Mountains", "type": 1 }, { "tag": "Geographic information system (GIS)", "type": 1 }, { "tag": "Geomorphological map", "type": 1 }, { "tag": "fluvial landforms", "type": 1 }, { "tag": "glacial landforms", "type": 1 }, { "tag": "karst landforms", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-05-12T15:09:12Z", "dateModified": "2017-05-12T15:09:12Z" } }, { "key": "H4XE3F4T", "version": 3780, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/H4XE3F4T", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/H4XE3F4T", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Evans et al.", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "H4XE3F4T", "version": 3780, "itemType": "journalArticle", "title": "Periglacial geomorphology of summit tors on Bodmin Moor, Cornwall, SW England", "creators": [ { "creatorType": "author", "firstName": "David J. A.", "lastName": "Evans" }, { "creatorType": "author", "firstName": "Ria", "lastName": "Kalyan" }, { "creatorType": "author", "firstName": "Chris", "lastName": "Orton" } ], "abstractNote": "Three maps are presented that portray the periglacial geomorphology of the three summit areas of Bodmin Moor, Cornwall, SW England, including Brown Willy (scale 1:2630), Kilmar/Bearah/Sharp tors (scale 1:3335) and Rough/Little Rough/Showery tors (scale 1:2175). Landform elements include castellated tors with well-developed cantilevered or precariously balanced corestones, summit blockfields, rock-fronted lobes thought to record former permafrost creep, patterned ground (stripes) and lower slope accumulations of crudely stratified growan or weathered granite residue. The altitudinal arrangement of these periglacial landforms appears to be a signature of a well-established periglacial landsystem and hence the Bodmin Moor granite massif is a suitable exemplar for a mature upland periglacial landsystem unaffected by glacierization.", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "novembre 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "342-349", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1308283", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1308283", "accessDate": "2017-04-20T16:21:19Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Bodmin Moor", "type": 1 }, { "tag": "Periglacial landsystem", "type": 1 }, { "tag": "Permafrost", "type": 1 }, { "tag": "rock-fronted lobes", "type": 1 }, { "tag": "tors", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-04-20T16:21:19Z", "dateModified": "2017-04-20T16:21:19Z" } }, { "key": "ADEHMP6C", "version": 3778, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/ADEHMP6C", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/ADEHMP6C", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Marra et al.", "parsedDate": "2017", "numChildren": 0 }, "data": { "key": "ADEHMP6C", "version": 3778, "itemType": "journalArticle", "title": "Using GIS in an Earth Sciences field course for quantitative exploration, data management and digital mapping", "creators": [ { "creatorType": "author", "firstName": "Wouter A.", "lastName": "Marra" }, { "creatorType": "author", "firstName": "Liesbeth van de", "lastName": "Grint" }, { "creatorType": "author", "firstName": "Koko", "lastName": "Alberti" }, { "creatorType": "author", "firstName": "Derek", "lastName": "Karssenberg" } ], "abstractNote": "Field courses are essential for subjects like Earth Sciences, Geography and Ecology. In these topics, GIS is used to manage and analyse spatial data, and offers quantitative methods that are beneficial for fieldwork. This paper presents changes made to a first-year Earth Sciences field course in the French Alps, where new GIS methods were introduced. Students use GIS in preparation to explore their research area using an elevation model and satellite images, formulate hypotheses and plan the fieldwork. During the fieldwork, a pilot group managed their field-observations using GIS and made digital maps. Students praise the use of quantitative digital maps in the preparation. Students made use of the available techniques during the fieldwork, although this could be further intensified. Some students were extra motivated due to the technical nature as well as the additional analytical possibilities. The use of GIS was experienced as a steep learning curve by students, and not all staff members are confident in supervising students using GIS, which calls for a sufficient preparation and training of both students and staff. The use of GIS adds abstract analyses and quantitative assessment, which is a complementary learning style to fieldwork that mostly focuses on practical skills.", "publicationTitle": "Journal of Geography in Higher Education", "publisher": "", "place": "", "date": "avril 3, 2017", "volume": "41", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "213-229", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/03098265.2017.1291587", "citationKey": "", "url": "http://dx.doi.org/10.1080/03098265.2017.1291587", "accessDate": "2017-03-31T12:47:28Z", "PMID": "", "PMCID": "", "ISSN": "0309-8265", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "GIS", "type": 1 }, { "tag": "Geomorphological mapping", "type": 1 }, { "tag": "Google Earth", "type": 1 }, { "tag": "QGIS", "type": 1 }, { "tag": "blended learning", "type": 1 }, { "tag": "fieldwork", "type": 1 } ], "collections": [ "I2BAT6CT", "UN94AR8C", "VTFPU8RG" ], "relations": {}, "dateAdded": "2017-03-31T12:47:28Z", "dateModified": "2017-03-31T12:47:28Z" } }, { "key": "KM3CJ7HZ", "version": 3771, "library": { "type": "group", "id": 4428, "name": "Eau et GEOpatrimoine-IGD", "links": { "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd", "type": "text/html" } } }, "links": { "self": { "href": "https://api.zotero.org/groups/4428/items/KM3CJ7HZ", "type": "application/json" }, "alternate": { "href": "https://www.zotero.org/groups/eau_et_geopatrimoine-igd/items/KM3CJ7HZ", "type": "text/html" } }, "meta": { "createdByUser": { "id": 40833, "username": "CedocIGUL", "name": "Centre de documentation (UNIL-IGD, CH)", "links": { "alternate": { "href": "https://www.zotero.org/cedocigul", "type": "text/html" } } }, "creatorSummary": "Tomczyk and Ewertowski", "parsedDate": "2017-11-30", "numChildren": 0 }, "data": { "key": "KM3CJ7HZ", "version": 3771, "itemType": "journalArticle", "title": "Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, Svalbard", "creators": [ { "creatorType": "author", "firstName": "Aleksandra M.", "lastName": "Tomczyk" }, { "creatorType": "author", "firstName": "Marek W.", "lastName": "Ewertowski" } ], "abstractNote": "A 1:19,500 map of the Petunibukta region documents the spatial distribution of almost 300 colluvial and alluvial fans (together with their catchments) in the periglacial high-Arctic environment of Svalbard. Fan-shaped landforms were mapped using an orthophoto and digital elevation model generated from 2009 aerial photographs and a 2013 high-resolution satellite image using Geographic Information Systems. Four additional maps at a scale of 1:40,000 provide details about the morphometric characteristics of the studied fans: long- and cross-profiles, slope and aspect. Additionally, parameters such as fan and catchment area, relief, length, width, elevation (the lowest point at the fan toe, apex, and the highest point of the catchment boundary), fan mean plan and profile curvatures, fan relation to neighbouring fans, are also presented. Fans were classified according to the dominant processes shaping their surface: colluvial fans (n = 229), alluvial fans dominated by debris flows (n = 49), and alluvial fans dominated by fluvial flows (n = 19).", "publicationTitle": "Journal of Maps", "publisher": "", "place": "", "date": "novembre 30, 2017", "volume": "13", "issue": "2", "section": "", "partNumber": "", "partTitle": "", "pages": "239-251", "series": "", "seriesTitle": "", "seriesText": "", "journalAbbreviation": "", "DOI": "10.1080/17445647.2017.1294543", "citationKey": "", "url": "http://dx.doi.org/10.1080/17445647.2017.1294543", "accessDate": "2017-03-09T14:24:59Z", "PMID": "", "PMCID": "", "ISSN": "null", "archive": "", "archiveLocation": "", "shortTitle": "", "language": "", "libraryCatalog": "Taylor and Francis+NEJM", "callNumber": "", "rights": "", "extra": "", "tags": [ { "tag": "Alluvial fan", "type": 1 }, { "tag": "Colluvial fan", "type": 1 }, { "tag": "GIS", "type": 1 }, { "tag": "Morphometry", "type": 1 }, { "tag": "Petuniabukta", "type": 1 }, { "tag": "Remote sensing", "type": 1 } ], "collections": [ "I2BAT6CT" ], "relations": {}, "dateAdded": "2017-03-09T14:24:59Z", "dateModified": "2017-03-09T14:24:59Z" } } ]