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            "title": "Geotourism and Geoeducation Potential of the Oyemekun Charnockitic Massif of Akure Area, Southwest Nigeria",
            "creators": [
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                    "creatorType": "author",
                    "firstName": "Olumuyiwa Michael",
                    "lastName": "Ajibade"
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                    "creatorType": "author",
                    "firstName": "Adegoke Olukayode",
                    "lastName": "Afolabi"
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                    "firstName": "Seun Damola",
                    "lastName": "Oladipupo"
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                    "firstName": "Tesleem Olalekan",
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                    "firstName": "Comfort Boluwaji",
                    "lastName": "Adegoke"
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                    "creatorType": "author",
                    "firstName": "Adedayo Abdullahi",
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            "abstractNote": "Animalia graphics in rocks are uncommon features that are rarely included as a component of geodiversity and hence largely undocumented. Unlike artificially carved petroglyphs, animalia rock arts, such as those observed at Oyemekun tourist centre, are natural imitations of animals formed by intrusive quartzofeldspathic veins within charnockite massifs. The Oyemekun massifs in Akure, occur within the southwestern part of the Precambrian Basement Complex of Nigeria. These massifs, dominated by high-grade charnockitic plutons, are exposed as inselbergs, whale-back hills, locally brecciated outcrops that are intruded by several quartzofeldspathic and pegmatitic veins. Field data revealed sharp lithologic contacts between these granitoids and the older and adjacent Archean to Early Proterozoic migmatite–gneiss while petrographical observations showed that the charnockites contained orthopyroxene (hypersthene), hornblende, biotite, quartz and plagioclase in a granoblastic groundmass, with zircon minerals occurring in accessory amounts. The pegmatitic quartzofeldspathic veins, ranging in size from a few millimetres to tens of centimetres, form graphic intergrowths mimicking animal shape-profiles such as patterns of dove, mermaid, and reptiles. Other geomorphologic rock art features of interest include inselbergs that outcropped as a whale with barnacles, the snout of a pig, and a dolphin imitation. Although, the Akure charnockite massif has been studied for its mineralogy, geochemistry and lithological association with other basement rocks, especially the migmatite gneiss complex, they have not been studied for their geotourism and geoconservation potential. This work presents the animalia graphic of the Oyemekun massifs and attempts to provide interpretive storytelling in the form of geoeducation materials that explain magma flow and viscosity as processes for the formation of these rock-art patterns. A geoconservation model is adapted to ensure protection from anthropogenic activities that may destroy this heritage.",
            "publicationTitle": "Geoheritage",
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            "date": "2025-12-03",
            "volume": "17",
            "issue": "4",
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            "pages": "176",
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            "journalAbbreviation": "Geoheritage",
            "DOI": "10.1007/s12371-025-01230-1",
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            "url": "https://doi.org/10.1007/s12371-025-01230-1",
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                    "tag": "Charnockite-animalia",
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            "title": "Etude morphosédimentaire et hydrologique du site emblématique du Gouffre à Plougrescant (Côtes-d’Armor, Bretagne) et perspectives de renaturation",
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                    "creatorType": "author",
                    "firstName": "Gillian",
                    "lastName": "Stéphan"
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                    "firstName": "Pierre",
                    "lastName": "Stéphan"
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                    "firstName": "Serge",
                    "lastName": "Suanez"
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                    "firstName": "Jérôme",
                    "lastName": "Ammann"
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                    "firstName": "Eloïse",
                    "lastName": "Thomas"
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                    "creatorType": "author",
                    "firstName": "Anne-Sophie",
                    "lastName": "Moreau"
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                    "creatorType": "author",
                    "firstName": "Éric",
                    "lastName": "Poulouin"
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                    "creatorType": "author",
                    "firstName": "Stéphane",
                    "lastName": "Riallin"
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            "abstractNote": "Le site du Gouffre à Plougrescant est un géotope breton inscrit à l’inventaire des objets géologiques remarquables (OGR) de Bretagne établi en 1994 par la Société Géologique et Minéralogique de Bretagne (SGMB). Ces caractéristiques géologiques et géomorphologiques remarquables ont contribué à sa mise en valeur touristique et culturelle par les collectivités locales à partir des années 1980. Aujourd’hui, le Conservatoire du littoral, en tant que gestionnaire du site, doit gérer les impacts d’une fréquentation qui ne cesse d’augmenter, et composer avec les aspirations/exigences d’une population riveraine installée sur cet espace depuis le XIXe siècle. Dans ce contexte, une étude morphosédimentaire des cordons de galets et des relations qu’ils entretiennent avec le fonctionnement hydrologique des lagunes rétrolittorales a été réalisée à la demande du Conservatoire du littoral. Le but de ce diagnostic est d’apporter des connaissances scientifiques pertinentes afin d’orienter/accompagner la politique de gestion et de renaturation du site. Si l’état morphologique et sédimentaire des cordons de galets ne présente aucune dégradation majeure, le fonctionnement hydrologique des lagunes a quant à lui été mis à mal par un ensemble d’interventions humaines. De toute évidence, il conviendra dans le futur d’intervenir sur ce point afin de redonner au site du Gouffre l’aspect naturel qui était le sien avant l’installation de l’Homme.",
            "publicationTitle": "Géomorphologie : relief, processus, environnement",
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            "date": "2025/08/01",
            "volume": "31",
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            "url": "https://journals.openedition.org/geomorphologie/20763",
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            "language": "fr",
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            "rights": "https://creativecommons.org/licenses/by-sa/4.0/",
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                    "tag": "Bretagne",
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                    "tag": "Gouffre (site du)",
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                    "tag": "cordons de galets",
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                    "tag": "lagunes",
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            "title": "Le Rhône aménagé vu du ciel. Constitution d'une base de données photographiques obliques pour documenter la trajectoire socio-environnementale du fleuve contemporain (1910-1960)",
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                    "creatorType": "author",
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            "abstractNote": "La photographie aérienne est un support très utilisé par les géographes pour reconstituer les dynamiques de changement des territoires. Bien que les clichés verticaux soient largement exploités dans les études géo-historiques, les clichés obliques, moins connus, offrent une meilleure perception des formes qui composent le paysage (relief, végétation, bâtiments) car l'angle de vue est plus proche de celui de nos yeux. Une base de données d'archives a été constituée dans le cadre de l'Observatoire Hommes-Milieux Vallée du Rhône, rassemblant des photographies aériennes obliques du corridor fluvial rhodanien et de ses affluents, issues du portail Remonter le temps de l'IGN. Un ensemble de 377 photographies obliques a été collecté du lac Léman à la mer Méditerranée entre 1919 et 1961, enrichi par des métadonnées détaillées et publié dans une photothèque interactive. Cet article de données présente les étapes de construction, les potentialités et les limites de la base de données. Les possibilités de réutilisation des photographies obliques par différentes disciplines scientifiques sont nombreuses. Elles représentent une opportunité unique d'enrichir les connaissances sur la trajectoire socio-environnementale de l'hydrosystème fluvial au cours du XX e siècle, d'éclairer l'histoire des aménagements et de comprendre les transformations paysagères profondes induites par l'urbanisation et l'industrialisation de la vallée du Rhône. Cette base de données d'archives offre également des supports de communication inédits pour le grand public et les acteurs des territoires.",
            "publicationTitle": "Data & Corpus. La revue des données en SHS",
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            "DOI": "10.46298/dc.15880",
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    {
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            "creatorSummary": "Richards et al.",
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            "title": "Map and Archival Evidence of the Historical Avulsion of the Brahmaputra River",
            "creators": [
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                    "creatorType": "author",
                    "firstName": "Keith",
                    "lastName": "Richards"
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                    "firstName": "Hugh",
                    "lastName": "Brammer"
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                    "creatorType": "author",
                    "firstName": "Patricia",
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            ],
            "abstractNote": "The Brahmaputra River is one of the world's largest rivers, entering the Bengal Basin from its extensive Himalayan catchment, flowing south through Bangladesh, and joining the Ganges to traverse a complex fan-delta and enter the Bay of Bengal. When Major James Rennell surveyed the river to establish the ‘Route Surveys’ for the East India Company between 1765 and 1777, it followed a different course, turning to the South-East into the Sylhet Basin, and joining the Meghna. Some time after this, it changed its course—it avulsed—and a re-survey was undertaken by Captain Richard Wilcox in 1828–1830 which first showed its present-day southerly route. However, there is uncertainty about when, why, and how this major adjustment occurred, and these questions can only be answered with recourse to archival materials. This paper accordingly pieces together information in the writings of travellers and East India Company officials in the region in the period between 1787 and 1854; evidence of boundary changes in 1806; archival material indicating that the East India Company was concerned enough about declining flow in the ‘Old’ Brahmaputra to consider engineering works by 1845; and contemporary evidence of the widespread impact of severe monsoon floods in 1787; to conclude that the avulsion probably took place rather earlier than often assumed. And intriguingly, it seems that although Rennell left India in 1777, in the first edition of his Memoir published after those floods had occurred (1788), he inserted a brief reference to the Brahmaputra changing its course.",
            "publicationTitle": "The Geographical Journal",
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            "date": "2025",
            "volume": "n/a",
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            "partNumber": "",
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            "pages": "e70059",
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            "DOI": "10.1111/geoj.70059",
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            "ISSN": "1475-4959",
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            "shortTitle": "",
            "language": "en",
            "libraryCatalog": "Wiley Online Library",
            "callNumber": "",
            "rights": "© 2025 The Author(s). The Geographical Journal published by John Wiley & Sons Ltd on behalf of Royal Geographical Society (with the Institute of British Geographers).",
            "extra": "_eprint: https://rgs-ibg.onlinelibrary.wiley.com/doi/pdf/10.1111/geoj.70059",
            "tags": [
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                },
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                    "tag": "East India Company",
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                    "tag": "James Rennell",
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                    "tag": "archival material",
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                    "tag": "monsoon floods",
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                    "tag": "river avulsion",
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            "title": "Mapping Africa's Climate Extremes: Delineation of Thermal Equator Under Current and Future Climate Scenarios",
            "creators": [
                {
                    "creatorType": "author",
                    "firstName": "Tabaro H.",
                    "lastName": "Kabanda"
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            ],
            "abstractNote": "The thermal equator, the latitudinal position of maximum mean annual surface temperature, represents a dynamic boundary in Earth's climate system. This study presents a high-resolution, longitudinally segmented analysis of Africa's thermal equator using CHELSA V2.1 baseline data and downscaled CMIP6 projections under the SSP3-7.0 scenario. I delineated the equator for 1981–2010, 2011–2040 and 2041–2070 and quantified shifts across longitudinal transects spaced at 0.5° intervals. Results show that under this scenario, by 2041–2070, thermal equator displacement is projected to exceed 300 km in several zones, with a mean latitudinal shift of 36.3 km. Hot spot analysis reveals that under the SSP3-7.0 scenario, persistent high-magnitude displacement clusters in Chad, with new hotspots projected to emerge in northeastern Central African Republic and central to southern Niger. Buffer-based overlays show increasing intersection with bare land (+28%) and arid ecoregions, while overlap with mesic biomes declines. These patterns reflect intensifying thermal gradients and spatially uneven climate reorganisation. The study provides a replicable framework for tracking surface thermal maxima at sub-continental scales and highlights emerging climate frontiers critical to ecosystem vulnerability, land degradation and regional adaptation planning.",
            "publicationTitle": "Geo: Geography and Environment",
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            "date": "2025",
            "volume": "12",
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            "pages": "e70039",
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            "ISSN": "2054-4049",
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            "shortTitle": "Mapping Africa's Climate Extremes",
            "language": "en",
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            "abstractNote": "Les glacières sont des cavités souterraines naturelles dans lesquelles de la glace formée il y a plusieurs siècles ou millénaires peut persister. Ces systèmes cryogéniques uniques se mettent en place dans des contextes géologiques, topographiques et climatiques spécifiques, qui favorisent l'accumulation et la conservation du froid hivernal tandis que la température moyenne annuelle de l’air en surface peut être positive. Contrairement aux glaciers, les masses de glace souterraines sont partiellement à l'abri des aléas climatiques immédiats, ce qui leur confère un rôle d’archives paléoenvironnementales. Fondé sur plus de 100 publications scientifiques, dont les 31 chapitres de l’ouvrage collectif de référence Ice Caves, cet article propose une synthèse des différentes dimensions de ces systèmes uniques : genèse, typologie morphodynamique, fonctionnement thermique, rôle d’archives paléoclimatiques et paléoenvironnementales, dimension patrimoniale, et menaces croissantes sur leur pérennité.",
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            "abstractNote": "Weather parameters and soil moisture profiles were measured at an hourly time step during four agricultural years (September to October, from 2018–19 to 2021–22) in two Jessour (water harvesting cultivated terraces) of the same valley in Zmerten (southeastern Tunisia), characterized by an arid climate. One instrumented Jesr (singular of Jessour) was located upstream and the other one downstream. During each dry season, when crops experience water stress, the downstream Jesr had a higher available water content than the upstream one; in the downstream Jesr the soil profile moisture remained above the wilting point, whereas in the upstream soil surface, moisture levels decreased to below the wilting point. High accumulation/low intensity rains (causing saturation/excess runoff) flooded both upstream and downstream Jessour from 50 mm of cumulative rainfall, whereas high intensity/low accumulation rains (causing infiltration/excess runoff) activated the downstream Jesr from an intensity of 15.2 mm/h, and a combination of moderate intensity and moderate accumulation rains activated both Jessour from an intensity of 8 mm/h and a cumulative rainfall of 33 mm. We propose to set 50 mm of cumulative rainfall and/or 6.4 mm/h of intensity as threshold values for the activation of the Jessour system in Zmerten. However, significant soil moisture recharges can occur even without activation of the Jessour system.",
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            "abstractNote": "The elements of geodiversity and their geoheritage are tangible materials that can be measured either qualitatively or quantitatively. This assessment involves a series of steps, starting with the inventory evaluation of their sites, considering the use or purpose that will be made of them. In the literature, there is a neglect of inventory sheet proposals for the evaluation of ex situ geodiversity, usually in the form of georesources used in the construction of Cultural Heritage. This article aims to present a model form, using as a case study the obelisk located within Independence Square, situated in the Historic Centre of João Pessoa, Paraíba, Northeast Brazil. This sheet is subdivided into five sections, covering all pertinent information about the mapped monument: framing, which names and locates the site; description of the location, with its means of access and characteristics of the place as a heritage asset; historical data; existing protection policy; and information on the geodiversity elements present. The obelisk at Independence Square has a well-known history and cultural importance, and as a result, receives a considerable number of visitors. However, the dissemination of Geosciences, through the study of georesources as elements of geodiversity involved in their constructions and ornamentations, can promote geoscientific education with a petrological approach.",
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            "title": "Proposed geoheritage sites along the transects of the Lunavada and surrounding areas promoting sustainable tourism within NE Gujarat and SW Rajasthan, India",
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            "abstractNote": "The Lunavada-Kadana Transect is an excellent area to display the geoheritage of the north-eastern region of Gujarat and south-western region of Rajasthan. It provides a diverse set of aspects to gawk at, stimulating the intrigue in one’s mind as well as bringing a heightened sense of appreciation for Earth processes. This paper provides a concise summary of four viable and easily accessible traverses across the region. The sites were selected after several detailed field seasons based on numerous factors such as individuality, scenic views, tourist attraction, peculiarity, uniqueness, and potential for tourism education as well as scientific studies. Additionally, they have been assessed with a quantitative scheme to determine their suitability for becoming geosites. The present study has narrowed down thirteen sites, which have a wide range of geological aspects. This variation in the range can promote the area to become a field geological museum and an arena to hone one’s field aptitude with a rich repository of literature published over the century. Such initiatives can also foster learning for sustainability by deepening our understanding of natural systems and encouraging responsible stewardship. Geosites are often overlooked and lost to the pages of obscurity buried within the pages of scientific literature; promoting them by granting the status of a Geoheritage site garners the attention of the masses as well as their appreciation for such features. Consequently, it becomes our duty to preserve such marvels as natural wealth for future generations through frameworks rooted in sustainable tourism and education for peace, ensuring that development is inclusive, mindful, and resilient.",
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                    "firstName": "Mohammad",
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            "abstractNote": "Les tables d’orientation réalisées par le Touring Club de France (TCF) au début du xxe siècle sont des dispositifs qui donnent à voir des représentations composites du paysage, sur des plateformes circulaires ou demi-circulaires réalisées en lave émaillée. Dans le cadre d’une recherche de doctorat menée entre paysage et design, nous nous attachons à explorer cette double dynamique propre aux tables d’orientation : tout à la fois dispositif déployé dans l’espace et représentation paysagère. Nous émettons l’hypothèse d’un point de rencontre entre espace et image institué par la table d’orientation, qui serait un « édifice-image ». Il s’agira de comprendre comment ces objets sont insérés in situ dans un territoire et comment ils agissent, simultanément, in visu, en produisant une représentation paysagère dans le temps même de la marche. À travers l’analyse d’un corpus de textes rédigés par les membres du TCF et leurs collaborateurs entre 1903 et 1938, nous nous concentrerons sur deux dispositifs qui apparaissent, à la lecture du corpus choisi, comme les prototypes des tables d’orientation dressées par le TCF. Nous nous pencherons d’abord sur le toposcope, dispositif de surveillance militaire particulièrement en usage au cours du xviiie siècle, puis sur l’indicateur des Alpes, dispositif d’exploration touristique des sommets au cœur des Alpes suisses, en usage tout au long du xixe siècle. Nous verrons en quoi ces deux dispositifs, par les deux types de points de vue sur le paysage qu’ils construisent, l’un militaire, l’autre contemplatif et instructif, donnent naissance aux tables d’orientation, poursuivant chacun à leur manière une quête de dépassement des limites du visible.",
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