Articles | Volume 17, issue 5
https://doi.org/10.5194/se-17-763-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-17-763-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Distributed right-lateral strain at the northern boundary of the Quito-Latacunga microblock
Nicolas Harrichhausen
CORRESPONDING AUTHOR
Department of Geological Sciences, University of Alaska Anchorage, Anchorage, USA
Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, IRD, Univ. Gustave Eiffel, ISTerre, Grenoble, France
Léo Marconato
Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, IRD, Univ. Gustave Eiffel, ISTerre, Grenoble, France
Laurence Audin
Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, IRD, Univ. Gustave Eiffel, ISTerre, Grenoble, France
Pierre Lacan
Instituto de Geociencias, Universidad Nacional Autónoma de México, Blvd. Juriquilla, 3001, 76230 Juriquilla, Querétaro, México
Géosciences Montpellier, University of Montpellier – CNRS, Montpellier, France
Stéphane Baize
Autorité de Sureté Nucléaire et de Radioprotection (ASNR), PSE-ENV/SCAN/BERSSIN, 92260, Fontenay aux Roses, France
Hervé Jomard
Autorité de Sureté Nucléaire et de Radioprotection (ASNR), PSE-ENV/SCAN/BERSSIN, 92260, Fontenay aux Roses, France
Alexandra Alvarado
Instituto Geofisico, Escuela Politécnica Nacional, Quito, Ecuador
James Hollingsworth
Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, IRD, Univ. Gustave Eiffel, ISTerre, Grenoble, France
Pierre-Henri Blard
CRPG, CNRS, Université de Lorraine, 54500, Vandoeuvre-lès-Nancy, France
Patricia Ann Mothes
Instituto Geofisico, Escuela Politécnica Nacional, Quito, Ecuador
Frédérique Rolandone
Sorbonne Université, CY, CNRS, ISTeP, Paris, France
Iván Dario Ortiz Martin
Servicio Geológico Colombiano, Bogotá, Colombia
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Nicolás Acuña Reyes, Léo Martin, Adrien Gilbert, Vincent Jomelli, Antoine Rabatel, Simon Filhol, Deborah Verfaillie, Pierre-Henri Blard, and Jérôme Lavé
EGUsphere, https://doi.org/10.5194/egusphere-2026-2638, https://doi.org/10.5194/egusphere-2026-2638, 2026
This preprint is open for discussion and under review for Climate of the Past (CP).
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Glacier landforms are often used to reconstruct past climate, but the same glacier shape can result from different combinations of temperature and snowfall. Using computer simulations of glaciers in the Bolivian Andes, we show that climate reconstructions based on a single glacier can lead to large uncertainties. By combining several neighboring glaciers, we estimate temperatures about 0.8°C cooler during the Little Ice Age and 1.3°C cooler during the Early Holocene (~10,000 years ago).
Daniel Martinez-Jaramillo, Sreeram-Reddy Kotha, F. Ramón Zúñiga, and Pierre Lacan
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2026-202, https://doi.org/10.5194/essd-2026-202, 2026
Preprint under review for ESSD
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This work presents a flatfile that quantifies how shaking is caused by earthquakes of different kinds. This could be used to predict the next shaking of the soil when an earthquake occurs, and then, help us to be prepared.
Gabriel Fénisse, Manuel Chevalier, Odile Peyron, David Vincent Bekaert, and Pierre-Henri Blard
EGUsphere, https://doi.org/10.5194/egusphere-2026-1590, https://doi.org/10.5194/egusphere-2026-1590, 2026
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Fossil pollen offers insights into past climates, yet results differ depending on reconstruction methods. By comparing multiple approaches across Europe during the Last Glacial Maximum, we highlight how method choice influences outcomes. Our work introduces a new methodological framework that reduces biases and improves the reliability of climate reconstructions.
Lisa Ardoin, Catherine Larose, Jean-Louis Tison, Christoph Keuschnig, Vasileios Gkinis, Saïda El Amri, Pierre-Henry Blard, Paul Bierman, Thomas Blunier, Dorthe Dahl-Jensen, Charlotte Maistriau, Jørgen-Peder Steffensen, Thomas Röckmann, and François Fripiat
EGUsphere, https://doi.org/10.5194/egusphere-2025-6204, https://doi.org/10.5194/egusphere-2025-6204, 2026
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We investigated gas dynamics at the ice–bed interface of two Greenland ice cores to assess methane and carbon dioxide behaviour beneath ice sheets. At Camp Century, methane diffuses into the ice and is partly oxidized. At GRIP, methane remains preserved despite oxygen. These contrasts suggest that methane oxidation is controlled by local basal conditions, including ice thickness and substrate availability.
Catherine M. Collins, Nicolas Perdrial, Pierre-Henri Blard, Nynke Keulen, William C. Mahaney, Halley Mastro, Juliana Souza, Donna M. Rizzo, Yves Marrocchi, Paul C. Knutz, and Paul R. Bierman
Clim. Past, 21, 1359–1381, https://doi.org/10.5194/cp-21-1359-2025, https://doi.org/10.5194/cp-21-1359-2025, 2025
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The Camp Century subglacial core stores information about past climates and glacial and interglacial processes in northwestern Greenland. In this study, we investigated the core archive, making large-scale observations using computed tomography (CT) scans and micron-scale observations observing physical and chemical characteristics of individual grains. We find evidence of past ice-free conditions, weathering processes during warmer periods, and past glaciations.
Paul R. Bierman, Andrew J. Christ, Catherine M. Collins, Halley M. Mastro, Juliana Souza, Pierre-Henri Blard, Stefanie Brachfeld, Zoe R. Courville, Tammy M. Rittenour, Elizabeth K. Thomas, Jean-Louis Tison, and François Fripiat
The Cryosphere, 18, 4029–4052, https://doi.org/10.5194/tc-18-4029-2024, https://doi.org/10.5194/tc-18-4029-2024, 2024
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In 1966, the U.S. Army drilled through the Greenland Ice Sheet at Camp Century, Greenland; they recovered 3.44 m of frozen material. Here, we decipher the material’s history. Water, flowing during a warm interglacial when the ice sheet melted from northwest Greenland, deposited the upper material which contains fossil plant and insect parts. The lower material, separated by more than a meter of ice with some sediment, is till, deposited by the ice sheet during a prior cold period.
Pedro Doll, Shaun Robert Eaves, Ben Matthew Kennedy, Pierre-Henri Blard, Alexander Robert Lee Nichols, Graham Sloan Leonard, Dougal Bruce Townsend, Jim William Cole, Chris Edward Conway, Sacha Baldwin, Gabriel Fénisse, Laurent Zimmermann, and Bouchaïb Tibari
Geochronology, 6, 365–395, https://doi.org/10.5194/gchron-6-365-2024, https://doi.org/10.5194/gchron-6-365-2024, 2024
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In this study, we use cosmogenic-sourced 3He to determine the eruption ages of 23 lava flows at Mt Ruapehu, Aotearoa New Zealand, and we show how this method can help overcome challenges associated with traditional dating methods in young lavas. Comparison with other methods demonstrates the accuracy of our data and the method's reliability. The new eruption ages allowed us to identify periods of quasi-simultaneous activity from different volcanic vents during the last 20 000 years.
Carole Petit, Tristan Salles, Vincent Godard, Yann Rolland, and Laurence Audin
Earth Surf. Dynam., 11, 183–201, https://doi.org/10.5194/esurf-11-183-2023, https://doi.org/10.5194/esurf-11-183-2023, 2023
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We present new tools in the landscape evolution model Badlands to simulate 10Be production, erosion and transport. These tools are applied to a source-to-sink system in the SW French Alps, where the model is calibrated. We propose a model that fits river incision rates and 10Be concentrations in sediments, and we show that 10Be in deep marine sediments is a signal with multiple contributions that cannot be easily interpreted in terms of climate forcing.
Agathe Defourny, Pierre-Henri Blard, Laurent Zimmermann, Patrick Jobé, Arnaud Collignon, Frédéric Nguyen, and Alain Dassargues
Hydrol. Earth Syst. Sci., 26, 2637–2648, https://doi.org/10.5194/hess-26-2637-2022, https://doi.org/10.5194/hess-26-2637-2022, 2022
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The Belgian city of Spa is known worldwide for its ferruginous and naturally sparkling groundwater springs that gave their name to the bathing tradition commonly called
spa. However, the origin of the dissolved CO2 they contain was still a matter of debate. Thanks to new analysis on groundwater samples, particularly carbon and helium isotopes together with dissolved gases, this study has demonstrated that the volcanic origin of the CO2 is presumably from the neighboring Eifel volcanic fields.
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Short summary
Tectonic plates can be broken into smaller blocks with deformation concentrated at their boundaries. We use remote sensing and field studies to investigate how faulting accommodates deformation at the northern boundary of the Quito-Latacunga microblock (Ecuador & Colombia). We show this boundary is a wide zone characterized by several parallel faults capable of hosting moderate to large (<M7) earthquakes, such as the one in 2022, and which may be influenced by nearby volcanism.
Tectonic plates can be broken into smaller blocks with deformation concentrated at their...