cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.22196950
title: Countermapping SDG 5 to address violence against women and girls in the favelas of Maré, Rio de Janeiro, Brazil

description: Violence Against Women and Girls (VAWG) remains one of the most significant problems affecting women globally with its elimination being central to achieving SDG 5 on gender equality. While information on its prevalence is increasing globally, this is often at the national scale with limited local-level data. Responding to feminist critiques of SDG 5 and target 5.2 in terms of the importance of capturing more nuanced data on grassroots women’s experiences as agents rather than victims, this paper reflects on countermapping VAWG in the favelas of Maré in Rio de Janeiro, Brazil. Drawing on countermapping methodologies, it analyses a series of countermaps highlighting the prevalence of VAWG, but also the need to report and resist it locally. Only by revealing the complexity of VAWG and women’s practices to deal with it can such violence be truly eliminated in order to meet SDG 5 and target 5.2.
DOI: 10.6084/m9.figshare.21308162.v1
title: Landscape evolution and the karst development in the Ojo Guareña multilevel cave system (Merindad de Sotoscueva, Burgos, Spain)

description: The Ojo Guareña karst system (OG) is located in the SE Cantabrian Range in northern Spain (Burgos, Spain). It is a multilevel cave system composed of 6 levels and is one of the longest cavities in the Iberian Peninsula (110 km). The spatial patterns and geomorphological characteristics of OG constitute a first-order record for studying the principal mechanisms of how the karst evolved by reconstruction and analysis of the external landscape. This extended karst system is attributed to the action of the local drainage system driven by Quaternary climatic fluctuations and lithological-structural controls. To contribute to this debate, we performed a detailed geomorphological mapping of this area (1:25,000 scale), differentiating the landforms according to the main geomorphological processes (structural, gravity, fluvial, glacial, weathering and polygenetic) involved. These datasets were used to draw a detailed geomorphological map and give a preliminary interpretation of the local landscape evolution.
DOI: 10.6084/m9.figshare.22730059
title: Reconstructing the historical shoreline evolution of the Northern Bay of Cádiz (SW Spain) from geomorphological and geoarchaeological data

description: During the last 3 ka, different human communities occupied the Bay of Cádiz (SW Spain), including Phoenician, Carthaginian, Roman, Medieval and Modern settlements. Traces of such historical occupations have been recognized along the bay from a geoarchaeological point of view. Some of them bear a palaeogeographical interest related to the historical location of the shoreline. At the same time, Holocene sedimentary units and geomorphological elements identified along the bay can be interpreted as evidences of its morphological evolution. The objective of the present paper is to represent all the available data about archaeological sites and geomorphology in the northern Bay of Cádiz, with the aim of combining both sources of data for elaborating a simple proposal of landscape evolution during the last 3 millennia. The base for mapping was multiple, from historical aerial photographs to satellite imagery and a digital terrain model with a maximum resolution of 0.35 m. .
DOI: 10.6084/m9.figshare.22730059.v1
title: Reconstructing the historical shoreline evolution of the Northern Bay of Cádiz (SW Spain) from geomorphological and geoarchaeological data

description: During the last 3 ka, different human communities occupied the Bay of Cádiz (SW Spain), including Phoenician, Carthaginian, Roman, Medieval and Modern settlements. Traces of such historical occupations have been recognized along the bay from a geoarchaeological point of view. Some of them bear a palaeogeographical interest related to the historical location of the shoreline. At the same time, Holocene sedimentary units and geomorphological elements identified along the bay can be interpreted as evidences of its morphological evolution. The objective of the present paper is to represent all the available data about archaeological sites and geomorphology in the northern Bay of Cádiz, with the aim of combining both sources of data for elaborating a simple proposal of landscape evolution during the last 3 millennia. The base for mapping was multiple, from historical aerial photographs to satellite imagery and a digital terrain model with a maximum resolution of 0.35 m. .
DOI: 10.6084/m9.figshare.23750793
title: Exploring the public bus ridership loss and recovery during the COVID-19 pandemic: a spatiotemporal analysis using smart card data

description: The COVID-19 pandemic has had a dramatic impact on the demand of public transport systems. Nevertheless, the global decrease and recovery of users has been uneven both in time and space. It is important to understand the extent of the unequal resilience of service areas with different characteristics. The objective of this study is to map the patterns of variations in the use of public bus at different scales, urban and regional. The data used were collected by an Automated Fare Collection system based on the use of smart travel cards in the Camp de Tarragona region (Southern Catalonia, Spain). Our approach has the potential to be applied in multiscale studies in other areas with similar data sources. This study also illustrates the potential that data generated by Automated Fare Collection systems have for a better understanding of uneven spatial and temporal patterns of public bus ridership during crises such as a pandemic. Data collected by Automated Fare Collection systems allow longitudinal analyses to be carried out at different scales and resolutions.Such analyses are key to understanding unequal territorial patterns and the evolution of the public bus system.Automated Fare Collection data can be used to measure the resilience of public bus to disruptions such as the COVID-19 pandemic.The construction of data visualizations can provide new insights in mobility studies, making them useful tools in the decision-making process. Data collected by Automated Fare Collection systems allow longitudinal analyses to be carried out at different scales and resolutions. Such analyses are key to understanding unequal territorial patterns and the evolution of the public bus system. Automated Fare Collection data can be used to measure the resilience of public bus to disruptions such as the COVID-19 pandemic. The construction of data visualizations can provide new insights in mobility studies, making them useful tools in the decision-making process.
DOI: 10.6084/m9.figshare.23750793.v1
title: Exploring the public bus ridership loss and recovery during the COVID-19 pandemic: a spatiotemporal analysis using smart card data

description: The COVID-19 pandemic has had a dramatic impact on the demand of public transport systems. Nevertheless, the global decrease and recovery of users has been uneven both in time and space. It is important to understand the extent of the unequal resilience of service areas with different characteristics. The objective of this study is to map the patterns of variations in the use of public bus at different scales, urban and regional. The data used were collected by an Automated Fare Collection system based on the use of smart travel cards in the Camp de Tarragona region (Southern Catalonia, Spain). Our approach has the potential to be applied in multiscale studies in other areas with similar data sources. This study also illustrates the potential that data generated by Automated Fare Collection systems have for a better understanding of uneven spatial and temporal patterns of public bus ridership during crises such as a pandemic. Data collected by Automated Fare Collection systems allow longitudinal analyses to be carried out at different scales and resolutions.Such analyses are key to understanding unequal territorial patterns and the evolution of the public bus system.Automated Fare Collection data can be used to measure the resilience of public bus to disruptions such as the COVID-19 pandemic.The construction of data visualizations can provide new insights in mobility studies, making them useful tools in the decision-making process. Data collected by Automated Fare Collection systems allow longitudinal analyses to be carried out at different scales and resolutions. Such analyses are key to understanding unequal territorial patterns and the evolution of the public bus system. Automated Fare Collection data can be used to measure the resilience of public bus to disruptions such as the COVID-19 pandemic. The construction of data visualizations can provide new insights in mobility studies, making them useful tools in the decision-making process.
DOI: 10.6084/m9.figshare.24355180
title: Prioritization of spatial protection of Šumava National Park, Czechia: comparing reality and the model

description: Natural processes and biodiversity are under pressure, especially in the human-dominated region of Central Europe. Therefore, an effective approach is needed for the conservation of the last fragments of valuable habitats. Šumava National Park is one of the biggest relatively natural forested areas within the cultural landscapes of Czechia and Central Europe. It has been protected since 1991 as a National Park, but management has been changed several times; thus, we would like to create a map with nature protection prioritization based on objective procedures and data to help manage the National Park with regard to its goals. We used occurrence data for 50 selected key fauna and flora species and made habitat suitability models; furthermore, data derived from the habitat mapping layer describing the quality of habitats were prepared. These data were inputs for prioritization ZONATION software resulting in a prioritization map, which could be compared with the current zonation of the National Park.
DOI: 10.6084/m9.figshare.24355180.v2
title: Prioritization of spatial protection of Šumava National Park, Czechia: comparing reality and the model

description: Natural processes and biodiversity are under pressure, especially in the human-dominated region of Central Europe. Therefore, an effective approach is needed for the conservation of the last fragments of valuable habitats. Šumava National Park is one of the biggest relatively natural forested areas within the cultural landscapes of Czechia and Central Europe. It has been protected since 1991 as a National Park, but management has been changed several times; thus, we would like to create a map with nature protection prioritization based on objective procedures and data to help manage the National Park with regard to its goals. We used occurrence data for 50 selected key fauna and flora species and made habitat suitability models; furthermore, data derived from the habitat mapping layer describing the quality of habitats were prepared. These data were inputs for prioritization ZONATION software resulting in a prioritization map, which could be compared with the current zonation of the National Park.
DOI: 10.6084/m9.figshare.21428186
title: Geology of giant quartz veins and their host rocks from the Eastern Pyrenees (Southwest Europe)

description: Giant Quartz Veins (GQVs) are ubiquitous in different tectonic settings and, besides being often related to hydrothermal ore deposits, also represent large-scale fingerprints of the structural and geochemical history of the rocks in which they are hosted. Here we present detailed geological maps and interpretations of three key areas of the Eastern Pyrenees where GQVs are well exposed. The studied rocks record different styles of deformation and are representative of common settings of the Pyrenees where GQVs are present: pre-Variscan metasedimentary and metavolcanic rocks, late Variscan granitoids, and Mesozoic and Cenozoic sedimentary rocks. GQVs in the study areas formed along pre-existing brittle and ductile structures or at locations with lithological heterogeneities, and have alteration haloes of silicified host rocks. The geological maps and interpretations presented here contribute to gain insights into the formation mechanisms of GQVs and into the structural constraints on fluid flow and mineral reactions at different depths of the Earth’s crust.
DOI: 10.6084/m9.figshare.21428186.v1
title: Geology of giant quartz veins and their host rocks from the Eastern Pyrenees (Southwest Europe)

description: Giant Quartz Veins (GQVs) are ubiquitous in different tectonic settings and, besides being often related to hydrothermal ore deposits, also represent large-scale fingerprints of the structural and geochemical history of the rocks in which they are hosted. Here we present detailed geological maps and interpretations of three key areas of the Eastern Pyrenees where GQVs are well exposed. The studied rocks record different styles of deformation and are representative of common settings of the Pyrenees where GQVs are present: pre-Variscan metasedimentary and metavolcanic rocks, late Variscan granitoids, and Mesozoic and Cenozoic sedimentary rocks. GQVs in the study areas formed along pre-existing brittle and ductile structures or at locations with lithological heterogeneities, and have alteration haloes of silicified host rocks. The geological maps and interpretations presented here contribute to gain insights into the formation mechanisms of GQVs and into the structural constraints on fluid flow and mineral reactions at different depths of the Earth’s crust.
DOI: 10.6084/m9.figshare.23200675
title: Geology of El Hierro Southern Rift, Canary Islands, Spain

description: The geological survey has been carried out in El Hierro with the aim to produce a new Geological Map at 1:12,500 scale for the Southern Rift. Almost 70 km<sup>2</sup> have been mapped providing a detailed stratigraphic and volcano-tectonic reconstruction of its evolution. Our work focused on the last Rift Volcanism phase, where hundreds of cinder cones, associated with thin lava flows, cover most of the island’s surface. Lava flows fields (40), monogenetic volcanic edifices (&gt;90), and volcano–tectonic structures (69), such as dykes, eruptive fissures, and faults have been surveyed and stored in the Geological Map. The map poses fundamental constraints on the Southern Rift geological evolution, mainly concerning its recent activity and allowing the definition of 4 main stages during the last 40 ka. Moreover, this 1:12,500 scale detailed map represents a primary tool for the volcanic hazard assessment of the Island, volcanic monitoring, urban planning, and further stratigraphic data-based investigations.
DOI: 10.6084/m9.figshare.23200675.v1
title: Geology of El Hierro Southern Rift, Canary Islands, Spain

description: The geological survey has been carried out in El Hierro with the aim to produce a new Geological Map at 1:12,500 scale for the Southern Rift. Almost 70 km<sup>2</sup> have been mapped providing a detailed stratigraphic and volcano-tectonic reconstruction of its evolution. Our work focused on the last Rift Volcanism phase, where hundreds of cinder cones, associated with thin lava flows, cover most of the island’s surface. Lava flows fields (40), monogenetic volcanic edifices (&gt;90), and volcano–tectonic structures (69), such as dykes, eruptive fissures, and faults have been surveyed and stored in the Geological Map. The map poses fundamental constraints on the Southern Rift geological evolution, mainly concerning its recent activity and allowing the definition of 4 main stages during the last 40 ka. Moreover, this 1:12,500 scale detailed map represents a primary tool for the volcanic hazard assessment of the Island, volcanic monitoring, urban planning, and further stratigraphic data-based investigations.
DOI: 10.6084/m9.figshare.23599820
title: Geologic map of the Terra Cimmeria-Nepenthes Mensae transitional zone, Mars – 1:1.45Million

description: A 1:1.45Million geologic map of NW Terra Cimmeria and SE Nepenthes Mensae (-5°31’–5°38’ N, 119°20’–129°55’ E) is presented here, displaying one of the highland-lowland transitional zones of Mars with greatest contrast and diversity. The Terra Cimmeria-Nepenthes Mensae Transitional Zone comprises two complex and poorly studied geologic domains bounded by the dichotomy escarpment. The map produced in this work displays nineteen geologic units and numerous geomorphic features. Detailed mapping, morphologic and morphometric analyses and Poisson model-derived ages have permitted to constrain the stratigraphy of this transitional zone and reconstruct more accurately its geological history from the Early Noachian to recent times, suggesting a significant period of fluvial activity within the Early Amazonian. The map provides insight into the processes involved in the origin and development of this transitional zone and offers a reference geologic framework for future studies in the region.
DOI: 10.6084/m9.figshare.23599820.v2
title: Geologic map of the Terra Cimmeria-Nepenthes Mensae transitional zone, Mars – 1:1.45Million

description: A 1:1.45Million geologic map of NW Terra Cimmeria and SE Nepenthes Mensae (-5°31’–5°38’ N, 119°20’–129°55’ E) is presented here, displaying one of the highland-lowland transitional zones of Mars with greatest contrast and diversity. The Terra Cimmeria-Nepenthes Mensae Transitional Zone comprises two complex and poorly studied geologic domains bounded by the dichotomy escarpment. The map produced in this work displays nineteen geologic units and numerous geomorphic features. Detailed mapping, morphologic and morphometric analyses and Poisson model-derived ages have permitted to constrain the stratigraphy of this transitional zone and reconstruct more accurately its geological history from the Early Noachian to recent times, suggesting a significant period of fluvial activity within the Early Amazonian. The map provides insight into the processes involved in the origin and development of this transitional zone and offers a reference geologic framework for future studies in the region.
DOI: 10.6084/m9.figshare.21320660
title: The influence of soil parameters on the price of agricultural land in Slovakia

description: The article analyses the relation of market prices in the agricultural land market and selected pedological characteristics of traded lands. During the period of 2009–2018 in 12 districts of Slovakia more than 153,000 plots with different pedo-ecological and geographic conditions have been analysed. Based on soil types, texture composition, steepness, gravel content, and depth, corresponding price levels were derived, and <i>soil price maps</i> were developed. The highest valued soils are of chernozem type (EUR 1.64 m<sup>−2</sup>), loamy soils (EUR 0.86 m<sup>−2</sup>), soils on flat land (EUR 1.09 m<sup>−2</sup>), slightly gravelly soils (EUR 1.02 m<sup>−2</sup>), and deep soils (EUR 1.10 m<sup>−2</sup>). The land price is evidently highly correlated with its qualitative parameters. Using GIS technologies, the entire territory of Slovakia has been categorized by this means and a so-called basic map of agricultural soil market prices in Slovakia has been created.
DOI: 10.6084/m9.figshare.21320660.v1
title: The influence of soil parameters on the price of agricultural land in Slovakia

description: The article analyses the relation of market prices in the agricultural land market and selected pedological characteristics of traded lands. During the period of 2009–2018 in 12 districts of Slovakia more than 153,000 plots with different pedo-ecological and geographic conditions have been analysed. Based on soil types, texture composition, steepness, gravel content, and depth, corresponding price levels were derived, and <i>soil price maps</i> were developed. The highest valued soils are of chernozem type (EUR 1.64 m<sup>−2</sup>), loamy soils (EUR 0.86 m<sup>−2</sup>), soils on flat land (EUR 1.09 m<sup>−2</sup>), slightly gravelly soils (EUR 1.02 m<sup>−2</sup>), and deep soils (EUR 1.10 m<sup>−2</sup>). The land price is evidently highly correlated with its qualitative parameters. Using GIS technologies, the entire territory of Slovakia has been categorized by this means and a so-called basic map of agricultural soil market prices in Slovakia has been created.
DOI: 10.6084/m9.figshare.23599820.v1
title: Geologic map of the Terra Cimmeria-Nepenthes Mensae transitional zone, Mars – 1:1.45Million

description: A 1:1.45Million geologic map of NW Terra Cimmeria and SE Nepenthes Mensae (-5°31’–5°38’ N, 119°20’–129°55’ E) is presented here, displaying one of the highland-lowland transitional zones of Mars with greatest contrast and diversity. The Terra Cimmeria-Nepenthes Mensae Transitional Zone comprises two complex and poorly studied geologic domains bounded by the dichotomy escarpment. The map produced in this work displays nineteen geologic units and numerous geomorphic features. Detailed mapping, morphologic and morphometric analyses and Poisson model-derived ages have permitted to constrain the stratigraphy of this transitional zone and reconstruct more accurately its geological history from the Early Noachian to recent times, suggesting a significant period of fluvial activity within the Early Amazonian. The map provides insight into the processes involved in the origin and development of this transitional zone and offers a reference geologic framework for future studies in the region.
DOI: 10.6084/m9.figshare.21864105
title: Geomorphology of the Central Kurdistan Region of Iraq: landscapes of the Erbil Plain between the Great Zab and Little Zab Rivers

description: We present the result of the geomorphological mapping of the central sector of the Kurdistan Region of Iraq. Therein, landscape evolution was mostly overseen by the regional geodynamic, related to the Arabia-Eurasia convergence, and in the Quaternary, regional climate fluctuations contributed to shaping landforms. The combination of such processes affected the distribution, types, and evolution of landforms (related to structural, hillslope, fluvial, and karst processes), with a noteworthy influence on the development of the local drainage network, which belongs to Tigris River catchment. The Great Zab and Little Zab Rivers – the main left tributaries of Tigris River – progressively cut anticline ridges growing in the area. Our analyses suggest that the structural deformation of the Zagros also controlled the evolution of the low-order channels of the hydrographic network. Since the Holocene, landforms dynamic was altered by intense human exploitation of the landscape and increased fluctuations between arid and humid conditions.
DOI: 10.6084/m9.figshare.21864105.v2
title: Geomorphology of the Central Kurdistan Region of Iraq: landscapes of the Erbil Plain between the Great Zab and Little Zab Rivers

description: We present the result of the geomorphological mapping of the central sector of the Kurdistan Region of Iraq. Therein, landscape evolution was mostly overseen by the regional geodynamic, related to the Arabia-Eurasia convergence, and in the Quaternary, regional climate fluctuations contributed to shaping landforms. The combination of such processes affected the distribution, types, and evolution of landforms (related to structural, hillslope, fluvial, and karst processes), with a noteworthy influence on the development of the local drainage network, which belongs to Tigris River catchment. The Great Zab and Little Zab Rivers – the main left tributaries of Tigris River – progressively cut anticline ridges growing in the area. Our analyses suggest that the structural deformation of the Zagros also controlled the evolution of the low-order channels of the hydrographic network. Since the Holocene, landforms dynamic was altered by intense human exploitation of the landscape and increased fluctuations between arid and humid conditions.