Articles | Volume 4, issue 2
https://doi.org/10.5194/gc-4-281-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gc-4-281-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
26 May 2021
Research article |
| 26 May 2021
| 26 May 2021
Using paired teaching for earthquake education in schools
Solmaz Mohadjer
CORRESPONDING AUTHOR
Department of Geosciences, University of Tübingen, Tübingen 72074, Germany
Earth and Environmental Sciences, University of Central Asia, Khorog 736000, Tajikistan
Sebastian G. Mutz
Department of Geosciences, University of Tübingen, Tübingen 72074, Germany
Matthew Kemp
Department of Earth Sciences, University of Oxford, Oxford OX1 3AN, United Kingdom
Sophie J. Gill
Department of Earth Sciences, University of Oxford, Oxford OX1 3AN, United Kingdom
Anatoly Ischuk
Institute of Geology, Earthquake Engineering and Seismology, Academy of Sciences of the Republic of Tajikistan, Dushanbe 734063, Tajikistan
Todd A. Ehlers
Department of Geosciences, University of Tübingen, Tübingen 72074, Germany
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In this manifesto, we offer six points of reflection that higher education geoscience educators can act upon to recognise and unlearn their biases and diversify the geosciences in higher education, complementing current calls for institutional and organisational change. This serves as a starting point to gather momentum to establish community-built opportunities for implementing and strengthening diversity, equity, inclusion, and justice holistically in geoscience education.
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Michael Dietze, Solmaz Mohadjer, Jens M. Turowski, Todd A. Ehlers, and Niels Hovius
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We use a seismometer network to detect and locate rockfalls, a key process shaping steep mountain landscapes. When tested against laser scan surveys, all seismically detected events could be located with an average deviation of 81 m. Seismic monitoring provides insight to the dynamics of individual rockfalls, which can be as small as 0.0053 m3. Thus, seismic methods provide unprecedented temporal, spatial and kinematic details about this important process.
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The Central Asia Fault Database is the first publicly accessible digital repository for active faults in central Asia and the surrounding regions. It includes an interactive map and a search tool that allow users to query and display critical fault information such as slip rates and earthquake history. The map displays over 1196 fault traces and 34 000 earthquake locations. The database contains attributes for 123 faults mentioned in the literature.
Shahzad Gani, Louise Arnal, Lucy Beattie, John Hillier, Sam Illingworth, Tiziana Lanza, Solmaz Mohadjer, Karoliina Pulkkinen, Heidi Roop, Iain Stewart, Kirsten von Elverfeldt, and Stephanie Zihms
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Science communication in geosciences has societal and scientific value but often operates in “shadowlands”. This editorial highlights these issues and proposes potential solutions. Our objective is to create a transparent and responsible geoscience communication landscape, fostering scientific progress, the well-being of scientists, and societal benefits.
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We applied the Maximum Entropy model to characterize multi-hazard scenarios in karst environments, focusing on flood-triggered sinkholes in Val d'Orléans, France. Karst terrains as multi-hazard forming areas, have received little attention in multi-hazard literature. Our study developed a multi-hazard susceptibility map to forecast the spatial distribution of these hazards. The findings improve understanding of hazard interactions and demonstrate the model's utility in multi-hazard analysis.
Mirjam Schaller, Daniel Peifer, Alexander B. Neely, Thomas Bernard, Christoph Glotzbach, Alexander R. Beer, and Todd A. Ehlers
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This study reports chemical weathering, physical erosion, and total denudation rates from river load data in the Swabian Alb, Southwest Germany. Tributaries to the Neckar River draining to the North show higher rates than tributaries draining to the South into the Danube River causing a retreat of the Swabian Alb escarpment. Observations are discussed in the light of lithology, climate, and topography. The data are further compared to other rates over space and time as well as to global data.
Valerio Poggi, Stefano Parolai, Natalya Silacheva, Anatoly Ischuk, Kanatbek Abdrakhmatov, Zainalobudin Kobuliev, Vakhitkhan Ismailov, Roman Ibragimov, Japar Karaev, Paola Ceresa, and Paolo Bazzurro
Nat. Hazards Earth Syst. Sci., 24, 2597–2613, https://doi.org/10.5194/nhess-24-2597-2024, https://doi.org/10.5194/nhess-24-2597-2024, 2024
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As part of the Strengthening Financial Resilience and Accelerating Risk Reduction in Central Asia (SFRARR) programme, funded by the European Union in collaboration with the World Bank and GFDRR, a regionally consistent probabilistic multi-hazard and multi-asset risk assessment has been developed. This paper describes the preparation of the input datasets (earthquake catalogue and active-fault database) required for the implementation of the probabilistic seismic hazard model.
Christoph Glotzbach and Todd A. Ehlers
Geochronology Discuss., https://doi.org/10.5194/gchron-2024-12, https://doi.org/10.5194/gchron-2024-12, 2024
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The (U-Th)/He dating method helps understand rock’s cooling history. Synthetic modeling experiments were conducted to explore factors affecting in-situ vs. whole-grain (U-Th)/He dates. In-situ dates are often 30 % older than whole-grain dates, whereas very rapid cooling makes helium loss negligible, resulting in similar whole-grain and in-situ dates. In addition, in-situ data can reveal cooling histories even from a single grain by measuring helium distributions.
Daniel Boateng, Sebastian G. Mutz, Armelle Ballian, Maud J. M. Meijers, Katharina Methner, Svetlana Botsyun, Andreas Mulch, and Todd A. Ehlers
Earth Syst. Dynam., 14, 1183–1210, https://doi.org/10.5194/esd-14-1183-2023, https://doi.org/10.5194/esd-14-1183-2023, 2023
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We present model-based topographic sensitivity experiments that provide valuable constraints for interpreting past proxies and records of climate and tectonic processes. The study uses a climate model to quantify the response of regional climate and oxygen isotopic composition of precipitation to diachronous surface uplift scenarios across the European Alps. The results suggest that isotopic signal changes can be measured in geologic archives using stable isotope paleoaltimetry.
Hemanti Sharma and Todd A. Ehlers
Earth Surf. Dynam., 11, 1161–1181, https://doi.org/10.5194/esurf-11-1161-2023, https://doi.org/10.5194/esurf-11-1161-2023, 2023
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Seasonality in precipitation (P) and vegetation (V) influences catchment erosion (E), although which factor plays the dominant role is unclear. In this study, we performed a sensitivity analysis of E to P–V seasonality through numerical modeling. Our results suggest that P variations strongly influence seasonal variations in E, while the effect of seasonal V variations is secondary but significant. This is more pronounced in moderate and least pronounced in extreme environmental settings.
Daniel Boateng and Sebastian G. Mutz
Geosci. Model Dev., 16, 6479–6514, https://doi.org/10.5194/gmd-16-6479-2023, https://doi.org/10.5194/gmd-16-6479-2023, 2023
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We present an open-source Python framework for performing empirical-statistical downscaling of climate information, such as precipitation. The user-friendly package comprises all the downscaling cycles including data preparation, model selection, training, and evaluation, designed in an efficient and flexible manner, allowing for quick and reproducible downscaling products. The framework would contribute to climate change impact assessments by generating accurate high-resolution climate data.
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Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-132, https://doi.org/10.5194/nhess-2023-132, 2023
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A regionally consistent probabilistic risk assessment for multiple hazards and assets was recently developed as part of the "Strengthening Financial Resilience and Accelerating Risk Reduction in Central Asia" (SFRARR) program, promoted by the European Union in collaboration with the World Bank and GFDRR. This paper describes the preparation of the source model and presents the main results of the probabilistic earthquake model for the Central Asian countries.
Hemanti Sharma, Sebastian G. Mutz, and Todd A. Ehlers
Earth Surf. Dynam., 10, 997–1015, https://doi.org/10.5194/esurf-10-997-2022, https://doi.org/10.5194/esurf-10-997-2022, 2022
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We estimate global changes in frost cracking intensity (FCI) using process-based models for four time slices in the late Cenozoic ranging from the Pliocene (∼ 3 Ma) to pre-industrial (∼ 1850 CE, PI). For all time slices, results indicate that FCI was most prevalent in middle to high latitudes and high-elevation lower-latitude areas such as Tibet. Larger deviations (relative to PI) were observed in colder (LGM) and warmer climates (Pliocene) due to differences in temperature and glaciation.
Caitlyn A. Hall, Sam Illingworth, Solmaz Mohadjer, Mathew Koll Roxy, Craig Poku, Frederick Otu-Larbi, Darryl Reano, Mara Freilich, Maria-Luisa Veisaga, Miguel Valencia, and Joey Morales
Geosci. Commun., 5, 275–280, https://doi.org/10.5194/gc-5-275-2022, https://doi.org/10.5194/gc-5-275-2022, 2022
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In this manifesto, we offer six points of reflection that higher education geoscience educators can act upon to recognise and unlearn their biases and diversify the geosciences in higher education, complementing current calls for institutional and organisational change. This serves as a starting point to gather momentum to establish community-built opportunities for implementing and strengthening diversity, equity, inclusion, and justice holistically in geoscience education.
Astrid Oetting, Emma C. Smith, Jan Erik Arndt, Boris Dorschel, Reinhard Drews, Todd A. Ehlers, Christoph Gaedicke, Coen Hofstede, Johann P. Klages, Gerhard Kuhn, Astrid Lambrecht, Andreas Läufer, Christoph Mayer, Ralf Tiedemann, Frank Wilhelms, and Olaf Eisen
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The maximal extent of grounded ice in this region was 11 km away from the continental shelf break.
The thickness of palaeo-ice on the calving front around the LGM was estimated to be at least 305 to 320 m.
We provide essential boundary conditions for palaeo-ice-sheet models.
Andrea Madella, Christoph Glotzbach, and Todd A. Ehlers
Geochronology, 4, 177–190, https://doi.org/10.5194/gchron-4-177-2022, https://doi.org/10.5194/gchron-4-177-2022, 2022
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Cooling ages date the time at which minerals cross a certain isotherm on the way up to Earth's surface. Such ages can be measured from bedrock material and river sand. If spatial variations in bedrock ages are known in a river catchment, the spatial distribution of erosion can be inferred from the distribution of the ages measured from the river sand grains. Here we develop a new tool to help such analyses, with particular emphasis on quantifying uncertainties due to sample size.
Mirjam Schaller and Todd A. Ehlers
Earth Surf. Dynam., 10, 131–150, https://doi.org/10.5194/esurf-10-131-2022, https://doi.org/10.5194/esurf-10-131-2022, 2022
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Soil production, chemical weathering, and physical erosion rates from the large climate and vegetation gradient of the Chilean Coastal Cordillera (26 to 38° S) are investigated. Rates are generally lowest in the sparsely vegetated and arid north, increase southward toward the Mediterranean climate, and then decrease slightly, or possible stay the same, further south in the temperate humid zone. This trend is compared with global data from similar soil-mantled hillslopes in granitic lithologies.
Emilija Krsnik, Katharina Methner, Marion Campani, Svetlana Botsyun, Sebastian G. Mutz, Todd A. Ehlers, Oliver Kempf, Jens Fiebig, Fritz Schlunegger, and Andreas Mulch
Solid Earth, 12, 2615–2631, https://doi.org/10.5194/se-12-2615-2021, https://doi.org/10.5194/se-12-2615-2021, 2021
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Here we present new surface elevation constraints for the middle Miocene Central Alps based on stable and clumped isotope geochemical analyses. Our reconstructed paleoelevation estimate is supported by isotope-enabled paleoclimate simulations and indicates that the Miocene Central Alps were characterized by a heterogeneous and spatially transient topography with high elevations locally exceeding 4000 m.
Kirstin Übernickel, Jaime Pizarro-Araya, Susila Bhagavathula, Leandro Paulino, and Todd A. Ehlers
Biogeosciences, 18, 5573–5594, https://doi.org/10.5194/bg-18-5573-2021, https://doi.org/10.5194/bg-18-5573-2021, 2021
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Animal burrowing is important because it impacts the physical and chemical evolution of Earth’s surface. However, most studies are species specific, and compilations of animal community effects are missing. We present an inventory of the currently known 390 burrowing species for all of Chile along its climate gradient. We observed increasing amounts of excavated material from an area with dry conditions along a gradient towards more humid conditions.
Sean D. Willett, Frédéric Herman, Matthew Fox, Nadja Stalder, Todd A. Ehlers, Ruohong Jiao, and Rong Yang
Earth Surf. Dynam., 9, 1153–1221, https://doi.org/10.5194/esurf-9-1153-2021, https://doi.org/10.5194/esurf-9-1153-2021, 2021
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The cooling climate of the last few million years leading into the ice ages has been linked to increasing erosion rates by glaciers. One of the ways to measure this is through mineral cooling ages. In this paper, we investigate potential bias in these data and the methods used to analyse them. We find that the data are not themselves biased but that appropriate methods must be used. Past studies have used appropriate methods and are sound in methodology.
Hemanti Sharma, Todd A. Ehlers, Christoph Glotzbach, Manuel Schmid, and Katja Tielbörger
Earth Surf. Dynam., 9, 1045–1072, https://doi.org/10.5194/esurf-9-1045-2021, https://doi.org/10.5194/esurf-9-1045-2021, 2021
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We study effects of variable climate–vegetation with different uplift rates on erosion–sedimentation using a landscape evolution modeling approach. Results suggest that regardless of uplift rates, transients in precipitation–vegetation lead to transients in erosion rates in the same direction of change. Vegetation-dependent erosion and sedimentation are influenced by Milankovitch timescale changes in climate, but these transients are superimposed upon tectonically driven uplift rates.
Joel C. Gill, Faith E. Taylor, Melanie J. Duncan, Solmaz Mohadjer, Mirianna Budimir, Hassan Mdala, and Vera Bukachi
Nat. Hazards Earth Syst. Sci., 21, 187–202, https://doi.org/10.5194/nhess-21-187-2021, https://doi.org/10.5194/nhess-21-187-2021, 2021
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This paper draws on the experiences of seven early career scientists, in different sectors and contexts, to explore the improved integration of natural hazard science into broader efforts to reduce the likelihood and impacts of disasters. We include recommendations for natural hazard scientists, to improve education, training, and research design and to strengthen institutional, financial, and policy actions. We hope to provoke discussion and catalyse changes that will help reduce disaster risk.
Mirjam Schaller, Igor Dal Bo, Todd A. Ehlers, Anja Klotzsche, Reinhard Drews, Juan Pablo Fuentes Espoz, and Jan van der Kruk
SOIL, 6, 629–647, https://doi.org/10.5194/soil-6-629-2020, https://doi.org/10.5194/soil-6-629-2020, 2020
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In this study geophysical observations from ground-penetrating radar with pedolith physical and geochemical properties from pedons excavated in four study areas of the climate and ecological gradient in the Chilean Coastal Cordillera are combined. Findings suggest that profiles with ground-penetrating radar along hillslopes can be used to infer lateral thickness variations in pedolith horizons and to some degree physical and chemical variations with depth.
Clemens Schannwell, Reinhard Drews, Todd A. Ehlers, Olaf Eisen, Christoph Mayer, Mika Malinen, Emma C. Smith, and Hannes Eisermann
The Cryosphere, 14, 3917–3934, https://doi.org/10.5194/tc-14-3917-2020, https://doi.org/10.5194/tc-14-3917-2020, 2020
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To reduce uncertainties associated with sea level rise projections, an accurate representation of ice flow is paramount. Most ice sheet models rely on simplified versions of the underlying ice flow equations. Due to the high computational costs, ice sheet models based on the complete ice flow equations have been restricted to < 1000 years. Here, we present a new model setup that extends the applicability of such models by an order of magnitude, permitting simulations of 40 000 years.
Clemens Schannwell, Reinhard Drews, Todd A. Ehlers, Olaf Eisen, Christoph Mayer, and Fabien Gillet-Chaulet
The Cryosphere, 13, 2673–2691, https://doi.org/10.5194/tc-13-2673-2019, https://doi.org/10.5194/tc-13-2673-2019, 2019
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Ice rises are important ice-sheet features that archive the ice sheet's history in their internal structure. Here we use a 3-D numerical ice-sheet model to simulate mechanisms that lead to changes in the geometry of the internal structure. We find that changes in snowfall result in much larger and faster changes than similar changes in ice-shelf geometry. This result is integral to fully unlocking the potential of ice rises as ice-dynamic archives and potential ice-core drilling sites.
Sebastian G. Mutz and Todd A. Ehlers
Earth Surf. Dynam., 7, 663–679, https://doi.org/10.5194/esurf-7-663-2019, https://doi.org/10.5194/esurf-7-663-2019, 2019
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We apply machine learning techniques to quantify and explain differences between recent palaeoclimates with regards to factors that are important in shaping the Earth's surface. We find that changes in ice cover, near-surface air temperature and rainfall duration create the most distinct differences. We also identify regions particularly prone to changes in rainfall and temperature-controlled erosion, which will help with the interpretation of erosion rates and geological archives.
Lorenz Michel, Christoph Glotzbach, Sarah Falkowski, Byron A. Adams, and Todd A. Ehlers
Earth Surf. Dynam., 7, 275–299, https://doi.org/10.5194/esurf-7-275-2019, https://doi.org/10.5194/esurf-7-275-2019, 2019
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Mountain-building processes are often investigated by assuming a steady state, meaning the balance between opposing forces, like mass influx and mass outflux. This work shows that the Olympic Mountains are in flux steady state on long timescales (i.e., 14 Myr), but the flux steady state could be disturbed on shorter timescales, especially by the Plio–Pleistocene glaciation. The contribution highlights the temporally nonsteady evolution of mountain ranges.
Matthias Nettesheim, Todd A. Ehlers, David M. Whipp, and Alexander Koptev
Solid Earth, 9, 1207–1224, https://doi.org/10.5194/se-9-1207-2018, https://doi.org/10.5194/se-9-1207-2018, 2018
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In this modeling study, we investigate rock uplift at plate corners (syntaxes). These are characterized by a unique bent geometry at subduction zones and exhibit some of the world's highest rock uplift rates. We find that the style of deformation changes above the plate's bent section and that active subduction is necessary to generate an isolated region of rapid uplift. Strong erosion there localizes uplift on even smaller scales, suggesting both tectonic and surface processes are important.
Manuel Schmid, Todd A. Ehlers, Christian Werner, Thomas Hickler, and Juan-Pablo Fuentes-Espoz
Earth Surf. Dynam., 6, 859–881, https://doi.org/10.5194/esurf-6-859-2018, https://doi.org/10.5194/esurf-6-859-2018, 2018
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We present a numerical modeling study into the interactions between transient climate and vegetation cover with hillslope and fluvial processes. We use a state-of-the-art landscape evolution model library (Landlab) and design model experiments to investigate the effect of climate change and the associated changes in surface vegetation cover on main basin metrics. This paper is a companion paper to Part 1 (this journal), which investigates the effect of climate change on surface vegetation cover.
Christian Werner, Manuel Schmid, Todd A. Ehlers, Juan Pablo Fuentes-Espoz, Jörg Steinkamp, Matthew Forrest, Johan Liakka, Antonio Maldonado, and Thomas Hickler
Earth Surf. Dynam., 6, 829–858, https://doi.org/10.5194/esurf-6-829-2018, https://doi.org/10.5194/esurf-6-829-2018, 2018
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Vegetation is crucial for modulating rates of denudation and landscape evolution, and is directly influenced by climate conditions and atmospheric CO2 concentrations. Using transient climate data and a state-of-the-art dynamic vegetation model we simulate the vegetation composition and cover from the Last Glacial Maximum to present along the Coastal Cordillera of Chile. In part 2 we assess the landscape response to transient climate and vegetation cover using a landscape evolution model.
Byron A. Adams and Todd A. Ehlers
Earth Surf. Dynam., 6, 595–610, https://doi.org/10.5194/esurf-6-595-2018, https://doi.org/10.5194/esurf-6-595-2018, 2018
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Where alpine glaciers were active in the past, they have created scenic landscapes that are likely in the process of morphing back into a form that it more stable with today's climate regime and tectonic forces. By looking at older erosion rates from before the time of large alpine glaciers and erosion rates since deglaciation in the Olympic Mountains (USA), we find that the topography and erosion rates have not drastically changed despite the impressive glacial valleys that have been carved.
Michelle E. Gilmore, Nadine McQuarrie, Paul R. Eizenhöfer, and Todd A. Ehlers
Solid Earth, 9, 599–627, https://doi.org/10.5194/se-9-599-2018, https://doi.org/10.5194/se-9-599-2018, 2018
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We examine the Himalayan Mountains of Bhutan by integrating balanced geologic cross sections with cooling ages from a suite of mineral systems. Interpretations of cooling ages are intrinsically linked to both the motion along faults as well as the location and magnitude of erosion. In this study, we use flexural and thermal kinematic models to understand the sensitivity of predicted cooling ages to changes in fault kinematics, geometry, and topography.
Sebastian G. Mutz, Todd A. Ehlers, Martin Werner, Gerrit Lohmann, Christian Stepanek, and Jingmin Li
Earth Surf. Dynam., 6, 271–301, https://doi.org/10.5194/esurf-6-271-2018, https://doi.org/10.5194/esurf-6-271-2018, 2018
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We use a climate model and statistics to provide an overview of regional climates from different times in the late Cenozoic. We focus on tectonically active mountain ranges in particular. Our results highlight significant changes in climates throughout the late Cenozoic, which should be taken into consideration when interpreting erosion rates. We also document the differences between model- and proxy-based estimates for late Cenozoic climate change in South America and Tibet.
Heiko Paeth, Christian Steger, Jingmin Li, Sebastian G. Mutz, and Todd A. Ehlers
Clim. Past Discuss., https://doi.org/10.5194/cp-2017-111, https://doi.org/10.5194/cp-2017-111, 2017
Manuscript not accepted for further review
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We use a high-resolution regional climate model to investigate various episodes of distinct climate states over the Tibetan Plateau region during the Cenozoic rise of the Plateau and Quaternary glacial/interglacial cycles. The simulated changes are in good agreement with available paleo-climatic reconstructions from proxy data. It is shown that in some regions of the Tibetan Plateau the climate anomalies during the Quaternary have been as strong as the changes occurring during the uplift period.
Michael Dietze, Solmaz Mohadjer, Jens M. Turowski, Todd A. Ehlers, and Niels Hovius
Earth Surf. Dynam., 5, 653–668, https://doi.org/10.5194/esurf-5-653-2017, https://doi.org/10.5194/esurf-5-653-2017, 2017
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We use a seismometer network to detect and locate rockfalls, a key process shaping steep mountain landscapes. When tested against laser scan surveys, all seismically detected events could be located with an average deviation of 81 m. Seismic monitoring provides insight to the dynamics of individual rockfalls, which can be as small as 0.0053 m3. Thus, seismic methods provide unprecedented temporal, spatial and kinematic details about this important process.
Solmaz Mohadjer, Todd Alan Ehlers, Rebecca Bendick, Konstanze Stübner, and Timo Strube
Nat. Hazards Earth Syst. Sci., 16, 529–542, https://doi.org/10.5194/nhess-16-529-2016, https://doi.org/10.5194/nhess-16-529-2016, 2016
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The Central Asia Fault Database is the first publicly accessible digital repository for active faults in central Asia and the surrounding regions. It includes an interactive map and a search tool that allow users to query and display critical fault information such as slip rates and earthquake history. The map displays over 1196 fault traces and 34 000 earthquake locations. The database contains attributes for 123 faults mentioned in the literature.
R. M. Headley and T. A. Ehlers
Earth Surf. Dynam., 3, 153–170, https://doi.org/10.5194/esurf-3-153-2015, https://doi.org/10.5194/esurf-3-153-2015, 2015
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Within a landscape evolution model operating over geologic timescales, this work evaluates how different assumptions and levels of complexity for modeling glacier flow impact the pattern and amount of glacial erosion. Compared to those in colder climates, modeled glaciers in warmer and wetter climates are more sensitive to the choice of glacier flow model. Differences between landscapes evolved with different glacier flow models are intensified over multiple cycles.
Related subject area
Subject: Geoscience education | Keyword: Pedagogy
The weather today rocks or sucks for my tree: exploring the understanding of climate impacts on forests at high school level through tweets
Climate Denial – the Antithesis of Climate Education: A Review
Arctic Tectonics and Volcanism: a multi-scale, multidisciplinary educational approach
The Rock Garden: a preliminary assessment of how campus-based field skills training impacts student confidence in real-world fieldwork
GC Insights: The crystal structures behind mineral properties – a case study of using TotBlocks in an undergraduate optical mineralogy lab
Building confidence in STEM students through breaking (unseen) barriers
The potential for using video games to teach geoscience: learning about the geology and geomorphology of Hokkaido (Japan) from playing Pokémon Legends: Arceus
Learning outcomes, learning support, and cohort cohesion on a virtual field trip: an analysis of student and staff perceptions
GC Insights: Diversifying the geosciences in higher education: a manifesto for change
A snapshot sample on how COVID-19 impacted and holds up a mirror to European water education
Virtual field experiences in a web-based video game environment: open-ended examples of existing and fictional field sites
GC Insights: Geoscience students' experience of writing academic poetry as an aid to their science education
GC Insights: Space sector careers resources in the UK need a greater diversity of roles
A remote field course implementing high-resolution topography acquisition with geomorphic applications
From a virtual field trip to geologically reasoned decisions in Yosemite Valley
Multi-scale virtual field experience: sedimentology and stratigraphy of Grand Ledge, Michigan, USA
Virtual mapping and analytical data integration: a teaching module using Precambrian crystalline basement in Colorado's Front Range (USA)
Virtual field trips as a tool for indirect geomorphological experience: a case study from the southeastern part of the Gulf of Corinth, Greece
Development and implementation of virtual field teaching resources: two karst geomorphology modules and three virtual capstone pathways
Evaluating participants' experience of extended interaction with cutting-edge physics research through the PRiSE “research in schools” programme
Schools of all backgrounds can do physics research – on the accessibility and equity of the Physics Research in School Environments (PRiSE) approach to independent research projects
A flexible, open, and interactive digital platform to support online and blended experiential learning environments: Thinglink and thin sections
Volcanoes in video games: the portrayal of volcanoes in commercial off-the-shelf (COTS) video games and their learning potential
Celebrating 25 years of seismology at schools in France
Thomas Mölg, Jan C. Schubert, Annette Debel, Steffen Höhnle, Kathy Steppe, Sibille Wehrmann, and Achim Bräuning
Geosci. Commun., 7, 215–225, https://doi.org/10.5194/gc-7-215-2024, https://doi.org/10.5194/gc-7-215-2024, 2024
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We examine the understanding of weather and climate impacts on forest health in high school students. Climate physics, tree ring science, and educational research collaborate to provide an online platform that captures the students’ observations, showing they translate the measured weather and basic tree responses well. However, students hardly ever detect the causal connections. This result will help refine future classroom concepts and public climate change communication on changing forests.
Gerald Kutney
EGUsphere, https://doi.org/10.5194/egusphere-2024-339, https://doi.org/10.5194/egusphere-2024-339, 2024
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This review examines the current state of global climate education, which shows that a problem exists and considers the causes and possible solutions. The problem does not appear to be climate education directly, or climate communication or climate science. Climate denial is the external force blunting the impact of climate education. Specific examples of climate denial in schools in North America and Europe are examined and how to deal with it.
Kim Senger, Grace Shephard, Fenna Ammerlaan, Owen Anfinson, Pascal Audet, Bernard Coakley, Victoria Ershova, Jan Inge Faleide, Sten-Andreas Grundvåg, Rafael Kenji Horota, Karthik Iyer, Julian Janocha, Morgan Jones, Alexander Minakov, Margaret Odlum, Anna M. R. Sartell, Andrew Schaeffer, Daniel Stockli, Marie A. Vander Kloet, and Carmen Gaina
Geosci. Commun. Discuss., https://doi.org/10.5194/gc-2024-3, https://doi.org/10.5194/gc-2024-3, 2024
Revised manuscript accepted for GC
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The article describes a course that we have developed at the University Centre in Svalbard that covers many aspects of Arctic Geology. The students experience this from a wide range of lecturers, focussing both on the small and larger scales, and covering many geoscientific disciplines.
Thomas W. Wong Hearing, Stijn Dewaele, Stijn Albers, Julie De Weirdt, and Marc De Batist
Geosci. Commun., 7, 17–33, https://doi.org/10.5194/gc-7-17-2024, https://doi.org/10.5194/gc-7-17-2024, 2024
Short summary
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Field skills training is an integral part of geoscience education, but long field courses away from home can be barriers to accessing that education and mean that students do not get regular field skills practice. We built the Rock Garden, an on-campus field course at Ghent University, Belgium, to make our field skills training more accessible. Here, we present preliminary data that suggest on-campus field skills training provision can increase students' confidence during real-world fieldwork.
Derek D. V. Leung and Paige E. dePolo
Geosci. Commun., 6, 125–129, https://doi.org/10.5194/gc-6-125-2023, https://doi.org/10.5194/gc-6-125-2023, 2023
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We used 3D-printed building blocks (TotBlocks) in an undergraduate optical mineralogy lab session to illustrate the links between crystal structures and the properties of minerals. Students built mica, pyroxene, and amphibole structures. We observed an improved understanding of cleavage (how minerals break) and pleochroism (how light interacts with minerals), but understanding did not improve with more abstract concepts. TotBlocks hold potential as a teaching tool in mineralogy classrooms.
Philip J. Heron and Jamie A. Williams
Geosci. Commun., 5, 355–361, https://doi.org/10.5194/gc-5-355-2022, https://doi.org/10.5194/gc-5-355-2022, 2022
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Science, technology, engineering, and maths subjects have historically struggled to be inclusive to students from diverse backgrounds. We outline here an outreach course designed to improve critical thinking for people in prison. Based on course feedback, we share advice for working with students who do not engage in formal education – specifically those who have low self-confidence. We focus on how to create a classroom dynamic that is accessible, inclusive and relatable to all students.
Edward G. McGowan and Lewis J. Alcott
Geosci. Commun., 5, 325–337, https://doi.org/10.5194/gc-5-325-2022, https://doi.org/10.5194/gc-5-325-2022, 2022
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The fictional landscape of Hisui from Pokémon Legends: Arceus is inspired by the real-world island of Hokkaido, Japan. This paper illustrates how the game can be used to explore geological concepts including volcanology, economic geology, and hazard mitigation, by comparing in-game features to their real-world counterparts on Hokkaido. Applications from this study include increasing geoscientific interest and facilitating the self-learning or formal teaching of geoscience worldwide.
Clare E. Bond, Jessica H. Pugsley, Lauren Kedar, Sarah R. Ledingham, Marianna Z. Skupinska, Tomasz K. Gluzinski, and Megan L. Boath
Geosci. Commun., 5, 307–323, https://doi.org/10.5194/gc-5-307-2022, https://doi.org/10.5194/gc-5-307-2022, 2022
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Virtual field trips are used to engage students who are unable to go into the field with geological field work. Here, we investigate the perceptions of staff and students before and after a virtual field trip, including the investigation of the success of mitigation measures designed to decrease barriers to engagement and inclusion. We conclude that negative and positive perceptions exist and that effective mitigation measures can be used to improve the student experience.
Caitlyn A. Hall, Sam Illingworth, Solmaz Mohadjer, Mathew Koll Roxy, Craig Poku, Frederick Otu-Larbi, Darryl Reano, Mara Freilich, Maria-Luisa Veisaga, Miguel Valencia, and Joey Morales
Geosci. Commun., 5, 275–280, https://doi.org/10.5194/gc-5-275-2022, https://doi.org/10.5194/gc-5-275-2022, 2022
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In this manifesto, we offer six points of reflection that higher education geoscience educators can act upon to recognise and unlearn their biases and diversify the geosciences in higher education, complementing current calls for institutional and organisational change. This serves as a starting point to gather momentum to establish community-built opportunities for implementing and strengthening diversity, equity, inclusion, and justice holistically in geoscience education.
Benjamin M. C. Fischer and Alexandru Tatomir
Geosci. Commun., 5, 261–274, https://doi.org/10.5194/gc-5-261-2022, https://doi.org/10.5194/gc-5-261-2022, 2022
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The aim of this paper is to communicate results of our survey giving a first overview and reflects how teaching of hydrology and water-related sciences changed due to COVID-19. Next to many negative aspects for teachers and students, a spirit of optimism, time of change and community initiatives could also be noticed. COVID-19 made it possible to explore novel teaching methods useful for modernizing education and making practical teaching formats accessible to all hydrology and water students.
Mattathias D. Needle, Juliet G. Crider, Jacky Mooc, and John F. Akers
Geosci. Commun., 5, 251–260, https://doi.org/10.5194/gc-5-251-2022, https://doi.org/10.5194/gc-5-251-2022, 2022
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We designed interactive, open-ended video games to simulate field geology to address the learning goals of traditional, in-person exercises for geology students. When these simulations were implemented in college courses, students used virtual versions of standard geology measuring tools to collect data but could also visualize and collect data in new ways (i.e., a jetpack and instantaneous graphing tools). The games were for remote learning, but the tools can also enhance in-person instruction.
Alice Wardle and Sam Illingworth
Geosci. Commun., 5, 221–225, https://doi.org/10.5194/gc-5-221-2022, https://doi.org/10.5194/gc-5-221-2022, 2022
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Participants answered four questions concerning their experience writing a haiku based on a geoscience extract. Data were categorised as being part of the
Task Processor
Task Meaning. The themes involved in the
Task Processwere
Identification of significant information,
Distillation of informationand
Metamorphosis of text, while the themes related to
Task Meaningwere made up of
Enjoyable,
Challenging(which has sub-themes
Frustratingand
Restricted) and
Valuable.
Martin O. Archer, Cara L. Waters, Shafiat Dewan, Simon Foster, and Antonio Portas
Geosci. Commun., 5, 119–123, https://doi.org/10.5194/gc-5-119-2022, https://doi.org/10.5194/gc-5-119-2022, 2022
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Educational research highlights that improved careers education is needed to increase participation in science, technology, engineering, and mathematics (STEM). Current UK careers resources in the space sector, however, are found to perhaps not best reflect the diversity of roles present and may in fact perpetuate misconceptions about the usefulness of science. We, therefore, compile a more diverse set of space-related jobs, which will be used in the development of a new space careers resource.
Sharon Bywater-Reyes and Beth Pratt-Sitaula
Geosci. Commun., 5, 101–117, https://doi.org/10.5194/gc-5-101-2022, https://doi.org/10.5194/gc-5-101-2022, 2022
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This paper outlines educational materials appropriate to teach upper division or graduate-level geoscience students how to produce and interpret high-resolution topography data. In a remote implementation, students were able to independently generate high-resolution topographic data products that can be used for interpreting hazards such as landsliding and flooding. Students met course learning outcomes while learning marketable skills used within environmental jobs or research settings.
Nicolas C. Barth, Greg M. Stock, and Kinnari Atit
Geosci. Commun., 5, 17–28, https://doi.org/10.5194/gc-5-17-2022, https://doi.org/10.5194/gc-5-17-2022, 2022
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We present a geology of Yosemite Valley virtual field trip (VFT) and companion exercises produced to substitute for physical field experiences. The VFT is created as an Earth project in Google Earth Web, a versatile format that allows access through a web browser. The module's progression from a VFT and a mapping exercise to geologically reasoned decision-making results in high-quality student work; students find it engaging, enjoyable, and educational.
Madeline S. Marshall and Melinda C. Higley
Geosci. Commun., 4, 461–474, https://doi.org/10.5194/gc-4-461-2021, https://doi.org/10.5194/gc-4-461-2021, 2021
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We created a virtual field trip (VFT) to Grand Ledge, a regionally important suite of outcrops in Michigan, USA. There is a wide range of sedimentary and stratigraphic features encompassed in this locality, making it ideal for a comprehensive virtual field experience. The VFT undertakes all stages of a field project: students investigate outcrops and samples at multiple scales, and students report successfully learning how to interpret complex sedimentary environments
like a real geologist.
Kevin H. Mahan, Michael G. Frothingham, and Ellen Alexander
Geosci. Commun., 4, 421–435, https://doi.org/10.5194/gc-4-421-2021, https://doi.org/10.5194/gc-4-421-2021, 2021
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We describe a virtual education module that encompasses many of the basic requirements of an advanced field exercise, including designing data collection strategies, synthesizing field and laboratory data, and communicating the results. Modules like the one shared here can successfully address some of the key learning objectives that are common to field-based capstone experiences while also fostering a more accessible and inclusive learning environment for all students.
Niki Evelpidou, Anna Karkani, Giannis Saitis, and Evangelos Spyrou
Geosci. Commun., 4, 351–360, https://doi.org/10.5194/gc-4-351-2021, https://doi.org/10.5194/gc-4-351-2021, 2021
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Field trips, despite their significance in students' education, cannot be performed under the COVID-19 pandemic. Here, we evaluate virtual field trips, as an alternative to in situ field work and as a means of preparation for live field trips, considering students' views. They are useful for geoscience students and a good alternative during restriction periods; although they can't substitute real field trips, they can be a valuable additional tool when preparing for a live field trip.
Rachel Bosch
Geosci. Commun., 4, 329–349, https://doi.org/10.5194/gc-4-329-2021, https://doi.org/10.5194/gc-4-329-2021, 2021
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In order to communicate the field-rich, complex concepts of karst geomorphology and hydrogeology to people who may not be able to access in-person field experiences, two virtual learning resources were created. Both karst activities, introductory and advanced, are available online in the Science Education Resource Center (SERC) Online Field Experiences repository. These and other activities from that SERC repository were incorporated into virtual capstone pathways for senior undergrad students.
Martin O. Archer, Jennifer DeWitt, Charlotte Thorley, and Olivia Keenan
Geosci. Commun., 4, 147–168, https://doi.org/10.5194/gc-4-147-2021, https://doi.org/10.5194/gc-4-147-2021, 2021
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We explore how best to support school students to experience undertaking research-level physics by evaluating provision in the PRiSE framework of
research in schoolsprojects. These experiences are received by students and teachers much more positively than typical forms of outreach. The intensive support offered is deemed necessary, with all elements appearing equally important. We suggest the framework could be adopted at other institutions applied to their own areas of scientific research.
Martin O. Archer
Geosci. Commun., 4, 189–208, https://doi.org/10.5194/gc-4-189-2021, https://doi.org/10.5194/gc-4-189-2021, 2021
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An evaluation of the accessibility and equity of a programme of independent research projects shows that, with the right support from both teachers and active researchers, schools' ability to succeed at undertaking cutting-edge research appears independent of typical societal inequalities.
Adam J. Jeffery, Steven L. Rogers, Kelly L. A. Jeffery, and Luke Hobson
Geosci. Commun., 4, 95–110, https://doi.org/10.5194/gc-4-95-2021, https://doi.org/10.5194/gc-4-95-2021, 2021
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We investigate the potential use of Thinglink, an interactive imagery-based web platform, for the study of rocks, minerals, and fossils under the microscope. We disseminated a prototype which allowed users to view rock samples through a "virtual" microscope and gathered feedback from staff and students. Results were overwhelmingly positive and imply real interest in this style of resource. Such resources could help to enhance accessibility and inclusivity and could complement existing teaching.
Edward G. McGowan and Jazmin P. Scarlett
Geosci. Commun., 4, 11–31, https://doi.org/10.5194/gc-4-11-2021, https://doi.org/10.5194/gc-4-11-2021, 2021
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Results from reviewing 15 popular video games demonstrate a combination of accuracies and inaccuracies that could impact on people’s self-learning of volcanoes. Several volcanic features are represented to varying degrees of accuracy (stratovolcanoes and calderas, lava flows, volcanic ash, and lava bombs), whereas health risks are often inaccurate. Suggested applications of the findings for educational environments are given, such as group projects in open-world games.
Jean-Luc Berenguer, Julien Balestra, Fabrice Jouffray, Fabrice Mourau, Françoise Courboulex, and Jean Virieux
Geosci. Commun., 3, 475–481, https://doi.org/10.5194/gc-3-475-2020, https://doi.org/10.5194/gc-3-475-2020, 2020
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An educational program, focusing on seismological activities at schools and on raising citizen awareness of natural hazards, has been active in France since 1995. Over this quarter century, different generations of students have learned various lessons concerning instrument installation, data recording, and analysis. Analysis of earthquakes has generated a strong awareness of the seismic hazard, especially after the deployment of seismometers at schools.
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Short summary
Lack of access to science-based natural hazards information impedes the effectiveness of school-based disaster risk reduction education. To address this challenge, we created and classroom tested a series of earthquake education videos that were co-taught by school teachers and Earth scientists in the UK and Tajikistan. Comparison of the results reveals significant differences between students' views on the Earth's interior and why and where earthquakes occur.
Lack of access to science-based natural hazards information impedes the effectiveness of...
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