Journal of Volcanology and Geothermal Research最新文献

{"title":"The crystalline silica respiratory hazard from rhyolitic lava dome eruptions in New Zealand's Taupo Volcanic Zone: A case study from the 1315 CE Kaharoa eruption","authors":"C.J. Horwell , H.M. Emerson , P. Ashwell , D.E. Damby , S. Self , C. Nattrass , R. Carey , B. Houghton","doi":"10.1016/j.jvolgeores.2025.108309","DOIUrl":"10.1016/j.jvolgeores.2025.108309","url":null,"abstract":"<div><div>The rhyolitic Kaharoa 1315 CE eruption was a complex, long-lived event from Tarawera volcano, New Zealand. Explosive phases were followed by around 5 years of lava dome extrusion and collapse which produced block-and-ash flows (BAF). Lava domes generate crystalline silica in the form of cristobalite, and rhyolitic magmas often contain quartz phenocrysts. Fine-grained ash containing crystalline silica can be formed through dome collapses or explosions, generating a respiratory health hazard for communities affected by ashfall. The aims of this study are to: i) determine whether the Kaharoa eruption dome-forming phase generated substantial quantities of crystalline silica and, therefore, to determine the potential for future dome-forming eruptions of Tarawera to do the same; ii) consider the potential hazard of the crystalline silica by studying the crystal habit and chemistry compared to other lava domes, globally; and iii) assess the particle size and crystalline silica content of the Kaharoa ash, to inform a respiratory hazard assessment.</div><div>Five co-BAF ash samples and one co-ignimbrite (explosive) ash sample from the Kaharoa pyroclastic deposits were analysed for health-pertinent factors: particle size distribution and crystalline silica content. Eight dome-rock samples were collected from the dome complex and associated BAF deposits and groundmass texture (especially forms of crystalline silica) and quantity of crystalline silica were assessed.</div><div>Cristobalite was present in the 4 ash samples analysed by X-ray diffraction (XRD; 1.3–3.7 wt%) as was quartz (5.7–12.5 wt%). For the 4 dome samples analysed by XRD, all samples contained quartz (4.1–10.4 wt%) and two contained significant quantities of cristobalite (24.7 and 27.3 wt%). Of the two dome samples with minimal cristobalite (visible as individual vapour-phase crystals by SEM but not quantifiable by XRD), one was from the non-devitrified dome carapace and the other was from the compacted interior but had not undergone devitrification. The two dome samples with substantial cristobalite were from dome interiors and were highly devitrified, with well-developed spherulitic textures. Using energy-dispersive X-ray spectroscopy, cristobalite in all samples contained minor aluminium, as has been seen for volcanic cristobalite from other lava domes, which may ameliorate its toxicity. By laser diffraction, the quantities of ash in the health pertinent size fractions varied, with a range of 1.3–8.1 vol% for particles of <4 μm diameter and 1.7–15.6 vol% for particles of <10 μm diameter, which is lower than measured in ash from large-scale dome collapse events at other volcanoes.</div><div>The findings suggest a potential for substantial crystalline silica to be formed in future Kaharoa-style eruptions, but that cristobalite generation is site-specific, depending on location within the dome and whether the dome remains sufficiently hot for spherulite formation and glass dev","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"461 ","pages":"Article 108309"},"PeriodicalIF":2.4,"publicationDate":"2025-03-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143580508","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Transition from growth to collapse of the Plinian column during the 1783 eruption of Asama volcano, Japan, inferred from rock microtextures","authors":"Tatsuki Mizuno ,&nbsp;Fukashi Maeno ,&nbsp;Atsushi Yasuda","doi":"10.1016/j.jvolgeores.2025.108310","DOIUrl":"10.1016/j.jvolgeores.2025.108310","url":null,"abstract":"<div><div>The 1783 eruption of Asama volcano was the most recent high-magnitude explosive eruption (VEI 4) in central Japan. During the climactic phase, the eruption transitioned from the formation of Plinian columns to the generation of pyroclastic density currents (PDCs). This study identified key differences in pyroclastic deposits across eruption styles, showing that changes in density, porosity, bubble microstructure, and water content. The pyroclastic fall deposits were divided into 14 layers of either pumice or ash, five of which contained silty ash derived from earlier PDCs. The pyroclastic fall deposits were overlain by PDC deposits generated in the climactic phase. Compared to fallout pumice, the PDC pumice had lower vesicularity and bubble connectivity but contained finer bubbles and high bubble number densities, suggesting higher magma decompression rates. Furthermore, the temperature and initial water content of the magma calculated from the compositions of the groundmass glasses and the crystals remained almost unchanged during the 1783 eruption, whereas the groundmass glass of the PDC pumice had a higher water content, indicating that the amount of water exsolved from the rising magma decreased. Based on theoretically predicted changes in vesicularity caused by water exsolution, we estimated that the mass fraction 0.81–0.93 of the initial water content was supplied to the plume during the formation of the climactic Plinian columns, and the mass fraction 0.68 during the PDC phase. The reduction in the water supply might have contributed to destabilizing the eruption column and caused the generation of PDCs.</div></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"462 ","pages":"Article 108310"},"PeriodicalIF":2.4,"publicationDate":"2025-03-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143682322","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"In one step: Insights into shallow differentiation from basalt to rhyolite at Cordón Caulle from rhyolite-MELTS simulations","authors":"Anna C. Ruefer ,&nbsp;Liam J. Kelly ,&nbsp;Guilherme A.R. Gualda ,&nbsp;Edgar L. Carrillo ,&nbsp;Sarah Hickernell ,&nbsp;Sarah Ward ,&nbsp;Heather Winslow ,&nbsp;Philipp Ruprecht","doi":"10.1016/j.jvolgeores.2025.108305","DOIUrl":"10.1016/j.jvolgeores.2025.108305","url":null,"abstract":"<div><div>Magma mush systems are commonly invoked as the source from which crystal-melt segregation produces rhyolites, but these systems are rarely observed. The 2011–2012 VEI 4 eruption of Cordón Caulle produced rhyolite lavas which scavenged basaltic enclaves. These enclaves contain interstitial glass similar to their host rhyolitic lava, suggesting that these enclaves offer a window into an active, shallow basaltic mush system. This mush was proposed as the source from which crystallization generates high-silica rhyolite in a single step. Here, we use rhyolite-MELTS to determine whether this is thermodynamically realistic. First, we use melt geobarometry to establish that enclave-derived pressures (∼25–200 MPa) are consistent with those previously determined for the lavas. We then simulate isobaric crystallization using a range of initial starting water concentrations to test if it is possible to generate rhyolites of the appropriate composition, assuming a starting composition which is the same as the basaltic enclave whole-rock. We find that it is possible to produce suitable rhyolitic compositions via fractional crystallization. We then explore the simulated physical consequences of crystallization and fluid exsolution. Lower water simulations (0.5–1.0 wt.% H₂O) at pressures of 100–200 MPa produce changes in volume most consistent with pre-eruptive ground deformation signals. We determine the timescales of heat loss from the crystallizing basaltic magma to be ∼8–25 ka, but it is plausible that heat loss occurred on the order of ∼1–10 ka which is broadly consistent with repose times of the system. The application of rhyolite-MELTS to an actively monitored system offers multifaceted insights into the geochemical, thermal, and physical evolution of magmas.</div></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"462 ","pages":"Article 108305"},"PeriodicalIF":2.4,"publicationDate":"2025-03-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143620067","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Evolution of the eruptive activity at Stromboli (Aeolian Islands - Italy) during the last 4 millennia. A tephrostratigraphic investigation on the early-phase of Recent Stromboli Eruptive Epoch","authors":"G. Re,&nbsp;Di Roberto Alessio,&nbsp;Del Carlo Paola,&nbsp;Pompilio Massimo","doi":"10.1016/j.jvolgeores.2025.108308","DOIUrl":"10.1016/j.jvolgeores.2025.108308","url":null,"abstract":"<div><div>Stromboli is famous for its persistent explosive activity that has been studied from various perspectives over the last century. By contrast, there is controversial information about the volcanic history regarding the period between 6000 years ago and the onset of the present-day activity.</div><div>Here, we present a comprehensive tephrostratigraphic investigation of the pyroclastic sequences that predate the onset of the present-day activity. This study integrates field observations, sedimentological analyses and radiometric ¹⁴C dating, together with detailed textural, petrographic and geochemical characterisation of juvenile clasts. Specifically, we document two superimposed volcaniclastic sequences, Member A and Member B, consisting of sub-conformable pyroclastic beds of lapilli and ash, interspersed with massive epiclastic deposits. While these sequences exhibit similar lithological features, indicating comparable eruptive dynamics, they are distinguishable for glass composition and chronostratigraphic framework.</div><div>In particular, a major change in the glass composition of the magma occurred after 1780 years ago, with a shift from high-K calc-alkaline (HKCA) to shoshonitic (SHO) affinity, composition that still persists in the present-day. We recognise four distinct eruptive periods with HKCA composition within Member A and two eruptive periods with SHO composition within Member B, both predating the onset of the present-day activity. Also, within Member A, we observed the earliest coexistence and mingling of two end-members with different texture and composition. This suggests that the feeding system of Stromboli could have been very similar to the present-day since at least 3200 years ago. It likely comprises two distinct magma bodies at different depths containing magmas with different compositions and porphyritic characteristics that occasionally interact prior to eruptions.</div><div>Our findings contribute to a comprehensive reconstruction of Stromboli's volcanic history and hold practical significance for anticipating and mitigating potential future volcanic events.</div></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"462 ","pages":"Article 108308"},"PeriodicalIF":2.4,"publicationDate":"2025-03-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143704582","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Gravity modeling of a prospective geothermal field of a hot spring in Western Saudi Arabia","authors":"Konstantinos Chavanidis ,&nbsp;Alexandros Stampolidis ,&nbsp;Ahmed Salem ,&nbsp;Abdul Latif Ashadi ,&nbsp;Abid Khogali ,&nbsp;Panagiotis Kirmizakis ,&nbsp;Pantelis Soupios","doi":"10.1016/j.jvolgeores.2025.108307","DOIUrl":"10.1016/j.jvolgeores.2025.108307","url":null,"abstract":"<div><div>The present study focuses on the geothermally prospective area of Wadi Al Lith (Western Saudi Arabia), which is expressed by the presence of hot springs. With a surface temperature that exceeds 80 °C, the Ain Al Harrah hot spring presents the most promising area for geothermal energy production. The Wadi Al Lith prospective geothermal field was generated by tectonic processes involved in the evolution of the Red Sea Rift. A land gravity survey of the area around the hot spring was conducted to develop a comprehensive model of the subsurface. The data were processed using the standard correction methods to construct the Bouguer anomaly map of the area, and the reservoir's 2D and 3D subsurface geometry was estimated. Our analysis revealed low gravity values at the hot spring site and high values in areas where the basement rocks are exposed. The 2D and 3D models were constrained and interpreted using available information from a shallow borehole and other geophysical methods (MT, TEM, and refraction seismic) that have been conducted in the area. The models suggest the possible existence of a geothermal reservoir by highlighting the tectonic structures and the fracture systems that facilitate the transport of thermal fluids to the surface. By reconstructing a detailed subsurface model of the Ain Al Harrah hot spring's surrounding area, the study highlights the potential of the Wadi Al Lith for renewable energy production. An exploratory and production drilling program is suggested, based on the interpretation of the geophysical data.</div></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"461 ","pages":"Article 108307"},"PeriodicalIF":2.4,"publicationDate":"2025-03-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143549851","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Viscosity of bubbly magmas from torsional experiments on pumice","authors":"Gaetano Ferrante ,&nbsp;Helge Gonnermann ,&nbsp;Céline Fliedner ,&nbsp;Thomas Giachetti ,&nbsp;Amy G. Ryan","doi":"10.1016/j.jvolgeores.2025.108297","DOIUrl":"10.1016/j.jvolgeores.2025.108297","url":null,"abstract":"<div><div>Bubbles in magma affect its viscosity, one of the most important properties for modeling volcanic eruptions. We performed new viscosity measurements on rhyolitic magma with bubble volume fractions, <span><math><mi>ϕ</mi></math></span>, between 0.15 and 0.80. Pumice samples from Medicine Lake Volcano, California, were deformed in torsion-compression experiments at a temperature of <span><math><mn>975</mn><msup><mspace></mspace><mo>°</mo></msup><mi>C</mi></math></span>, and strains up to ∼3. Capillary numbers during the experiments were large and viscosity, <span><math><mi>η</mi></math></span>, decreased with increasing <span><math><mi>ϕ</mi></math></span>. The experiments have coherent trends in <span><math><mi>η</mi></math></span> vs. <span><math><mi>ϕ</mi></math></span> with little scatter. We define a new constitutive relation for the relative viscosity of bubbly rhyolitic melt, <span><math><msub><mi>η</mi><mi>r</mi></msub><mo>=</mo><mo>exp</mo><mfenced><mrow><mn>5.5</mn><mspace></mspace><mi>ϕ</mi><mo>/</mo><mfenced><mrow><mn>2</mn><mo>−</mo><mi>ϕ</mi></mrow></mfenced></mrow></mfenced><mo>,</mo></math></span> and for bubbly suspensions at high Capillary numbers in general, reducing the uncertainties associated with scatter among the the body of prior experiments. Our results are useful for more robust modeling of volcanic eruptions.</div></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"461 ","pages":"Article 108297"},"PeriodicalIF":2.4,"publicationDate":"2025-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143549852","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Progressive drying of the hydrothermal system of La Soufrière de Guadeloupe (French West Indies) revealed by multi-year monitoring of chlorine isotopic composition of fumarolic HCl","authors":"Étienne Le Glas ,&nbsp;Magali Bonifacie ,&nbsp;Roberto Moretti ,&nbsp;Vincent Robert ,&nbsp;Pierre Agrinier ,&nbsp;Jabrane Labidi ,&nbsp;Gérard Bardoux ,&nbsp;Laëtitia Pantobe ,&nbsp;Arnaud Burtin ,&nbsp;Élodie Chillin-Eusebe ,&nbsp;Tristan Didier ,&nbsp;Manuel Inostroza","doi":"10.1016/j.jvolgeores.2025.108306","DOIUrl":"10.1016/j.jvolgeores.2025.108306","url":null,"abstract":"<div><div>Closed-conduit volcanoes develop hydrothermal aquifers where infiltrating waters dissolve magmatic gases such as SO₂, HCl, and HF. The extent of this “scrubbing effect” is traditionally tracked using CO₂/SO₂ or CO₂/S_Total, but these ratios can also be modified by secondary processes. Given the high solubility of gaseous HCl_(g) into aqueous water, we assess here chlorine isotopic compositions (δ³⁷Cl) in fumarolic HCl_(g) as a potential quantitative index of scrubbing.</div><div>We present three years and a half (January 2018 to May 2021) of δ³⁷Cl and chlorine concentrations [Cl] data from fumarolic gases at La Soufrière de Guadeloupe, alongside traditional geochemical tracers in volcanology. Our data show strong negative correlation between δ³⁷Cl and [Cl] values, suggesting variable extents of HCl dissolution into the hydrothermal aquifer through time. High δ³⁷Cl values associated to low [Cl] indicate intense ³⁵Cl loss into the aquifer, while low δ³⁷Cl values with high [Cl] likely reflect more pristine magmatic signatures with minimal extents of scrubbing.</div><div>The observed δ³⁷Cl–[Cl] trends suggest Cl isotopic fractionation factors between gas and liquid Δ_g-l varying between +2.5 and +5 ‰. These values are higher than expected at equilibrium, suggesting kinetic fractionations likely resulting from rapid gas flow (preventing isotopic equilibration with liquid water). The fact that comparable δ³⁷Cl–[Cl] trends are found at Poás (Costa Rica) and Vulcano (Italy) suggests that such kinetic fractionations during HCl scrubbing may be widespread.</div><div>Comparisons between δ³⁷Cl and CO₂/CH₄ ratios and the modeled groundwater level within the dome suggest that variations in scrubbing at La Soufrière are primarily driven by varying magmatic inputs. The progressive decrease in δ³⁷Cl, associated with increasing [Cl] from 2019 to 2021, likely reflects long-term aquifer drying, predating the observed rise in fumarolic temperatures above 150 °C in mid-2023.</div></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"462 ","pages":"Article 108306"},"PeriodicalIF":2.4,"publicationDate":"2025-02-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143628377","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Geological history of Samodiva Mons shield volcano, and surrounding area, Quadrangle V-29, Venus","authors":"D.G. Malyshev ,&nbsp;R.E. Ernst ,&nbsp;H. El Bilali ,&nbsp;M.A. Ivanov ,&nbsp;C.H.G. Braga ,&nbsp;V.E. Rozhin ,&nbsp;A.S. Shimolina","doi":"10.1016/j.jvolgeores.2025.108296","DOIUrl":"10.1016/j.jvolgeores.2025.108296","url":null,"abstract":"<div><div>Samodiva Mons is a large shield volcano (∼240 km in diameter, centered at 13.6° N, 291.0° E) located 1500 km ESE from Beta Regio. Detailed mapping (1:500,000 scale) using radar image and altimetry data from the Magellan mission was used to investigate the geological history of the volcano and its surrounding area. The study area is located in Quadrangle V-29, which extends from 11° to 16° N, 289° to 294° E and covers approximately 291,000 km² of which ∼80,000 km² is occupied by Samodiva Mons volcanic materials. Seven geological units were defined, mapped, and characterized: Samodiva Mons lava flows, small shield volcanoes, coronae material, plains material, tesserae, densely lineated plains, and impact craters. Also, we distinguished two structural units: graben-fissure systems (interpreted as dike swarms) and wrinkle ridges. Three geological stages of evolution of the study region are recognized, with Stages 1–2 being pre-Samodiva Mons and Stage 3 that is associated with Samodiva Mons activity. This stage largely postdates the emplacement of regional plains and was culminated by the formation of the Samodiva Mons volcanic construct.</div></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"461 ","pages":"Article 108296"},"PeriodicalIF":2.4,"publicationDate":"2025-02-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143463861","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Dynamics of tephra fallout and column collapse during Plinian eruptions of Mt. Pelée volcano (Lesser Antilles): The 2.5 ka cal BCE P5 eruption","authors":"Guillaume Carazzo ,&nbsp;Audrey Michaud-Dubuy ,&nbsp;Vincent Bellier ,&nbsp;Benoit Vittecoq","doi":"10.1016/j.jvolgeores.2025.108295","DOIUrl":"10.1016/j.jvolgeores.2025.108295","url":null,"abstract":"<div><div>Mt. Pelée volcano in Martinique (Lesser Antilles) has undergone volcanic unrest since 2019 and an increase of alert level to yellow (vigilance) in 2020. Historical records and field studies show that this volcano has produced numerous dome-forming and sub-Plinian to Plinian eruptions over the last 25 kyr. The 2.5 ka cal BCE P5 eruption dispersed lapilli and ash across the northern part of Martinique. Here, we present field data on tephra dispersal and grain-size distribution to estimate the eruption source parameters and reconstruct the dynamical evolution of the eruption. Our results show that after a short opening phase, the P5 Plinian eruption formed a 26 km-high stable column with a northeastern dispersal axis. The total volume of the eruption is estimated to be 0.39 ± 0.03 km³ DRE making P5 a VEI 4 event. The mass eruption rate increased from ≈ 1.1 × 10⁸ kg s⁻¹ to ≈ 4.8 × 10⁸ kg s⁻¹ leading to column collapse and the formation of pyroclastic density currents on the flanks of the volcano. The transition from stable column to collapse occurred at conditions well predicted by a 1D model of volcanic plumes and confirms that this eruptive scenario is recurrent at Mt. Pelée volcano over the last 5 kyr. The tephra dispersal of the P5 eruptive products reinforces the accuracy of the current hazard map and provides volcanological constraints to better assess volcanic hazards in the Lesser Antilles.</div></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"461 ","pages":"Article 108295"},"PeriodicalIF":2.4,"publicationDate":"2025-02-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143453023","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Comprehensive orientation method using cross-line laser: A case study of paleomagnetic analysis on pyroclastic deposits from Asama Volcano (Japan)","authors":"Tatsuo Kanamaru ,&nbsp;Kuniyuki Furukawa ,&nbsp;Akari Maki","doi":"10.1016/j.jvolgeores.2025.108293","DOIUrl":"10.1016/j.jvolgeores.2025.108293","url":null,"abstract":"<div><div>Accurate orientation of terrestrial materials is essential in earth sciences, particularly in structural geology and paleomagnetic studies. In this study, we present a novel and versatile sample orientation method utilizing commercially available cross-line lasers. This method address challenges in collecting oriented geological samples caused by factors such as sample size, fragility, rough surfaces, and local magnetic anomalies that complicate the use of magnetic compasses. To evaluate the effectiveness of this method, paleomagnetic measurements were performed on juvenile clasts from pyroclastic density current deposits and the pyroclastic fall deposit of the 1783 eruption of Asama Volcano. The result coincides within error limits with the geomagnetic field predicted by a paleosecular variation curve, demonstrating the potential of our orienting method. However, further experiments are required to quantify the precision of our orienting method and to assess its dependence on factors such as clast size and shape. Preliminary paleomagnetic analyses of the pyroclastic fall deposit suggest a complex emplacement history and indicate a surprisingly high-temperature emplacement. These findings offer new insights into the emplacement processes and thermal history of pyroclastic deposits. This innovative method enhances the capability to collect and analyze oriented geological samples, providing significant contributions to volcanological and structural geological research.</div></div>","PeriodicalId":54753,"journal":{"name":"Journal of Volcanology and Geothermal Research","volume":"461 ","pages":"Article 108293"},"PeriodicalIF":2.4,"publicationDate":"2025-02-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143421907","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}