Готові списки джерел за темами / Landslide and debris flow

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Добірка наукової літератури з теми "Landslide and debris flow"

Автор: Grafiati

Опубліковано: 3 червня 2025

Оновлено: 31 липня 2025

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Статті в журналах з теми "Landslide and debris flow"

Tsuchiya, Satoshi, and Fumitoshi Imaizumi. "Large Sediment Movement Caused by the Catastrophic Ohya-Kuzure Landslide." Journal of Disaster Research 5, no. 3 (2010): 257–63. http://dx.doi.org/10.20965/jdr.2010.p0257.

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The Ohya-kuzure landslide, one of three largest catastrophic landslides in Japan, is assumed to have been triggered by a strong earthquake and a large-scale debris terrace in a channel downstream from landslide. We verified the time of the landslide’s occurrence, its volume, and the amount of sediment supplied to the main river downstream. The landslide’s occurrence in 1707 was confirmed by historical documents and earthquake records of sediment disasters. The landslide’s size was estimated to be 94 million m3, from the geomorphic change in the debris terrace. Moreover, it was presumed that 33

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Bobrova, Darya, Ekaterina Kazakova, Svetlana Rybalchenko, and Sergei Kudriavtcev. "Debris flow and landslide processes on manmade landscapes." MATEC Web of Conferences 265 (2019): 04009. http://dx.doi.org/10.1051/matecconf/201926504009.

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Currently the human activity is one of the important factors of debris flow and landslide formation. In some cases, human activity leads to the formation of previously non-existing debris flow and landslide complexes, which increases the areal percentage of exposure of settlement areas to dangerous processes. Most often, anthropogenic debris flows and landslides are confined to the mountainous territory, which is associated with the extraction of minerals, road construction, construction of buildings and structures and storage of soil in floodplains and watercourses on weak mountain slopes. Th

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Brien, Dianne L., Mark E. Reid, Collin Cronkite-Ratcliff, and Jonathan P. Perkins. "Topographic controls on landslide mobility: modeling hurricane-induced landslide runout and debris-flow inundation in Puerto Rico." Natural Hazards and Earth System Sciences 25, no. 3 (2025): 1229–53. https://doi.org/10.5194/nhess-25-1229-2025.

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Abstract. In 2017, Hurricane Maria triggered more than 70 000 landslides in Puerto Rico. After initiation, these predominantly shallow landslides were mobilized to varying extents – some landslides only traveled partway downslope, whereas others reached drainage channels and were mobilized into long-traveled debris flows that could severely impact roads and infrastructure. Thus, forecasting potential landslide runout and inundation zones is critical for estimating landslide and debris-flow hazards. Here we conduct an in-depth topographic analysis of landslide-affected areas from nine study are

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Liang, Zhu, Changming Wang, Donghe Ma, and Kaleem Ullah Jan Khan. "Exploring the potential relationship between the occurrence of debris flow and landslides." Natural Hazards and Earth System Sciences 21, no. 4 (2021): 1247–62. http://dx.doi.org/10.5194/nhess-21-1247-2021.

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Abstract. The present study is to explore the potential relationship between debris flow and landslides by establishing susceptibility zoning maps (SZMs) separately with the use of random forest (RF). Lhünzê county, located in southeastern Tibet, was selected as the study area. The work was carried out with the following steps: (1) an inventory map consisting of 399 landslides and 49 debris flows was determined; (2) slope units and 11 conditioning factors were prepared for the susceptibility modeling of landslide while watershed units and 12 factors were prepared for debris flow; (3) SZMs were

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Hasnawir, Hasnawir. "EARLY WARNING OF RAINFALL-INDUCED LANDSLIDES AND DEBRIS FLOWS ON MT. BAWAKARAENG, SOUTH SULAWESI,INDONESIA." JOURNAL OF FORESTRY RESEARCH 10, no. 1 (2013): 1–10. https://doi.org/10.20886/ijfr.2013.10.1.1-10.

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Rainfall thresholds that form the basis of the landslide warning systems now exist for a few areas in Indonesia. Based on analysis of historical data, threshold performance varies according to precipitation characteristics,  and threshold  exceed corresponds  to a given probability  of  landslide occurrence. Early warnings of landslides and debris flows that include specific information about affected areas, probability of landslide and debris flow occurrence, and expected timing are technically feasible as illustrated by a case study made on Mt. Bawakaraeng, South Sul

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Wan, Baofeng, Ning An, and Gexue Bai. "Monitoring and Evaluation of Debris Flow Disaster in the Loess Plateau Area of China: A Case Study." Water 16, no. 17 (2024): 2539. http://dx.doi.org/10.3390/w16172539.

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The Loess Plateau area, with complex geomorphological features and geological structure, is highly prone to geologic disasters such as landslides and debris flow, which cause great losses. To investigate the initiation mechanism of landslide and debris flow disasters and their spreading patterns, historical satellite images in the Laolang gully were collected and digitized to generate three-dimensional topographic and geomorphological maps. Typical landslides were selected for landslide thickness measurement using a standard penetrometer and high-density electrical method. Numerical models wer

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Kwan, Julian SH, and H. W. Sun. "An improved landslide mobility model." Canadian Geotechnical Journal 43, no. 5 (2006): 531–39. http://dx.doi.org/10.1139/t06-010.

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A relatively simple and versatile numerical model known as DAN, developed by Oldrich Hungr for the assessment of landslide mobility, has been enhanced to incorporate the consideration of a trapezoidal-shaped flow channel for more realistic modelling purposes. This enhanced debris mobility model (DMM) has been programmed to run on a spreadsheet and has been calibrated against detailed landslide data in Hong Kong. In contrast to previous work, the enhanced DMM eliminates the limitations inherited from the assumption of a rectangular flow channel with frictionless side boundaries. When using DMM,

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Ahmed, Shahid, Muhammad Ishtiaq, Baoliang Lu, and Khadim Hussain. "LANDSLIDE MAPPING AND SPATIAL DISTRIBUTION ANALYSIS FROM MUZAFFARABAD TO LUAT AREA WITH CASE STUDY OF PLANG LANDSLIDE, LESSER HIMALAYAS, PAKISTAN." Geological Behavior 7, no. 2 (2023): 88–99. http://dx.doi.org/10.26480/gbr.02.2023.88.99.

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Landslides are one of the most dangerous and frequent natural hazards worldwide and in Pakistan, wreaking havoc on society and the economy. Susceptibility mapping, as well as geological and geotechnical investigations, are the focus of this study on the Plang landslide in Neelam Valley, Pakistan’s Lesser Himalayas. This landslide’s causes and solutions were determined by a combination of geotechnical soil testing, longitudinal profiles, geological mapping, seismicity, roadcut, and rainfall assessments. The greatest concentration of landslides (as measured by both number of occurrences and slop

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Gao, Ruiyuan, Changming Wang, Zhu Liang, Songling Han, and Bailong Li. "A Research on Susceptibility Mapping of Multiple Geological Hazards in Yanzi River Basin, China." ISPRS International Journal of Geo-Information 10, no. 4 (2021): 218. http://dx.doi.org/10.3390/ijgi10040218.

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Collapses, landslides, and debris flows are the main geological hazards faced by mankind, which bring heavy losses of life and property to people every year. The purpose of this paper is to establish a method for determining the optimal weighting scheme for multiple geological hazard susceptibility mapping. The information gain ratio (IGR) method was used to analyze the predictive ability of the conditioning factors. The support vector machine (SVM) algorithm was used to evaluate the susceptibility to collapse, landslide, and debris flow of the study area. The receiver operating characteristic

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Komu, Muge Pinar, Hakan Ahmet Nefeslioglu, and Candan Gokceoglu. "Modeling Shallow Landslide Runout Distance in Eocene Flysch Facies Using Empirical–Statistical Models (Western Black Sea Region of Türkiye)." ISPRS International Journal of Geo-Information 13, no. 3 (2024): 84. http://dx.doi.org/10.3390/ijgi13030084.

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Uncertainties related to runout distances in shallow landslide analyses may not only affect lives but may also result in economic losses. Owing to the increase in shallow landslides, which are especially triggered by heavy rainfall, runout distances have been investigated to decipher whether applications of a functional runout distance are feasible. This paper aims to give insights into the modeling of the shallow landslide runout probability in Eocene flysch facies in the Western Black Sea region of Türkiye. There are two main stages in this study—which are dominated by empirical models, the

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Дисертації з теми "Landslide and debris flow"

Paudel, Bhuwani Prasad. "GIS-based Assessment of Debris Flow Susceptibility and Hazard in Mountainous Regions of Nepal." Thesis, Université d'Ottawa / University of Ottawa, 2019. http://hdl.handle.net/10393/38817.

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Rainfall-induced landslides that change into debris flows and travel large distances are one of the treacherous natural calamities that can occur in mountainous areas, particularly in Nepal’s mountains. Debris flow was the second highest cause of human death in Nepal after epidemics between 1971 and 2016. Because debris flow is common in mountainous regions, its prediction and remedial measures through land use plans are important factors to consider for saving lives and properties. The spatial distribution of the initial landslides that change into debris flow, on a watershed scale, is still

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Awal, Ripendra. "Study on Landslide Dam Failure Due to Sliding and Overtopping." 京都大学 (Kyoto University), 2008. http://hdl.handle.net/2433/66199.

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Kyoto University (京都大学) 0048 新制・課程博士 博士(工学) 甲第14136号 工博第2970号 新制||工||1441(附属図書館) 26442 UT51-2008-N453 京都大学大学院工学研究科社会基盤工学専攻 (主査)教授中川一, 教授関口秀雄, 教授藤田正治 学位規則第4条第1項該当

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Zhao, Tao. "Investigation of landslide-induced debris flows by the DEM and CFD." Thesis, University of Oxford, 2014. http://ora.ox.ac.uk/objects/uuid:316cb3fc-dfc6-4e5a-bc0d-298e298c9c5b.

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In recent years, the increasing impacts of landslide hazards on human lives and lifeline facilities worldwide has advanced the necessity to find out both economically acceptable and useful techniques to predict the occurrence and destructive power of landslides. Though many projects exist to attain this goal, the current investigation set out to establish an understanding of the initiation and propagation mechanisms of landslides via numerical simulations, so that mitigation strategies to reduce the long-term losses from landslide hazards can be made. In this research, the Discrete Element Met

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McGuire, Luke A., Francis K. Rengers, Jason W. Kean, et al. "Elucidating the role of vegetation in the initiation of rainfall-induced shallow landslides: Insights from an extreme rainfall event in the Colorado Front Range." AMER GEOPHYSICAL UNION, 2016. http://hdl.handle.net/10150/621986.

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More than 1100 debris flows were mobilized from shallow landslides during a rainstorm from 9 to 13 September 2013 in the Colorado Front Range, with the vast majority initiating on sparsely vegetated, south facing terrain. To investigate the physical processes responsible for the observed aspect control, we made measurements of soil properties on a densely forested north facing hillslope and a grassland-dominated south facing hillslope in the Colorado Front Range and performed numerical modeling of transient changes in soil pore water pressure throughout the rainstorm. Using the numerical model

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Wishart, Jeremy Scott. "Overtopping Breaching of Rock-Avalanche Dams." Thesis, University of Canterbury. Civil Engineering, 2007. http://hdl.handle.net/10092/1193.

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River blockages formed by rock avalanches appear to pose a higher hazard potential than other landslide dams, given the extreme run-out distances and volumes of rock avalanche deposits. Recent research has identified rock avalanche deposits to have internal sedimentology consisting of a coarse surficial material (carapace) and a finer fragmented interior (body) potentially of critical importance to rock-avalanche dam stability. Physical scale modelling of overtopping failure and breach development in rock avalanche dams was used to quantify the influence of this sedimentology on critical breac

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Peres, David Johnny. "The hydrologic control on shallow landslide triggering: empirical and monte carlo pysically-based approaches." Doctoral thesis, Università di Catania, 2013. http://hdl.handle.net/10761/1387.

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In the dissertation, a Monte Carlo approach, that combines stochastic and deterministic modeling approaches, is used to analyze the hydrological control on shallow landslide triggering. In particular, an integrated stochastic rainfall and deterministic landslide simulator has been developed for the purpose. The simulator is composed by the following components: (i) a seasonal Neyman-Scott Rectangular Pulses (NRSP) model to generate synthetic hourly point rainfall data; (ii) a module for rainfall event identification and separation from dry intervals; (iii) the Transient Rainfall Infiltratio

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Festa, Davide. "Debris flow susceptibility mapping for initiation areas at medium scale: a case study in Western Norway." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2019. http://amslaurea.unibo.it/18141/.

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In recent years, rapid mass movements such as debris flow and debris avalanches resulted in a significant impact on Norwegian society and economy. The need for dispelling the uncertainty inherent in landslide risk assessment has encouraged the development of hazard and susceptibility maps. Different statistically-based modelling methods, in combination with geographic information systems (GIS), have been extensively used to ascertain landslide susceptibility in quantitative terms. This thesis proposes a bivariate statistical method (Weights of Evidence) for assessing the spatial pronenes

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Milne, Fraser Dalton. "Topographic and material controls on the Scottish debris flow geohazard." Thesis, University of Dundee, 2008. https://discovery.dundee.ac.uk/en/studentTheses/eb4a6b03-8024-4818-8e92-ce1fd3c77209.

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Debris flows can be considered the most significant geological hazard in areas of high relief in Scotland having impacted upon slope foot infrastructure several times in recent years. The potency of this geohazard is anticipated to increase over the coming decades due to a climatologically enforced upturn in debris flow frequency. In thisresearch material and topographic controls on debris flow activity are investigated using a combination of field and laboratory based analysis of debris flows at six study sites across upland Scotland. Centrifuge modelling is also used to simulate theinitiatio

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Palau, Berastegui Rosa Maria. "Landslide and debris flow warning at regional scale. A real-time system using susceptibility mapping, radar rainfall and hydrometeorological thresholds." Doctoral thesis, Universitat Politècnica de Catalunya, 2021. http://hdl.handle.net/10803/672681.

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Rainfall triggered shallow slides and debris flows constitute a significant hazard that causes substantial economic losses and fatalities worldwide. Regional-scale risk mitigation for these processes is challenging. Therefore, landslide early warning systems (LEWS) are a helpful tool to depict the time and location of possible landslide events so that the hazardous situation can be managed more effectively. The main objective of this thesis is to set up a regional-scale LEWS that works in real-time over Catalonia (NE Spain). The developed warning system combines in real-time susceptibility in

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BLAHUT, JAN. "Debris flow hazard and risk analysis at medium and local scale." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2010. http://hdl.handle.net/10281/10914.

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Increased population, its wealth and activities lead to increased risk from landslide hazards in the mountain areas. The presented study deal with the analysis of debris flow hazard and risk at medium (regional) and local (site-specific) scale. Study took place in part of Valtellina Valley in Italian Central Alps. The first part of the study presents information about landslide hazard, risk and debris flow processes. It also shows historical information about natural disasters in the study area of Mountain Consortium of Municipalities of Valtellina di Tirano together with the results from a g

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Книги з теми "Landslide and debris flow"

Gori, Paula. Debris-flow hazards in the Blue Ridge of Virginia. U.S. Geological Survey, 1996.

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Gori, Paula. Debris-flow hazards in the Blue Ridge of Virginia. U.S. Geological Survey, 1996.

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Gori, Paula. Debris-flow hazards in the Blue Ridge of Virginia. U.S. Geological Survey, 1996.

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Gori, Paula. Debris-flow hazards in the Blue Ridge of Virginia. U.S. Geological Survey, 1996.

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Gori, Paula. Debris-flow hazards in the Blue Ridge of Virginia. U.S. Geological Survey, 1996.

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Gori, Paula. Debris-flow hazards in the Blue Ridge of Virginia. U.S. Geological Survey, 1996.

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Gori, Paula. Debris-flow hazards in the Blue Ridge of Virginia. U.S. Geological Survey, 1996.

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Landslide Hazard Reduction Program (Geological Survey), ed. A model for grain flow and debris flow. U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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L, Ellis William, Kibler D. F. 1940-, and Geological Survey (U.S.), eds. Results of site investigation and instrumentation of the Keno Gulch landslide/debris-flow source area, Aspen, Colorado. U.S. Dept. of the Interior, U.S. Geological Survey, 1997.

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Zhao, Tao. Coupled DEM-CFD Analyses of Landslide-Induced Debris Flows. Springer Singapore, 2017. http://dx.doi.org/10.1007/978-981-10-4627-8.

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Частини книг з теми "Landslide and debris flow"

Zerkal, Oleg V., Sergey S. Chernomorets, Viktoriia A. Iudina, et al. "The Modern Activity of the Buzulgan Landslide and Its Influence on the Debris Flow Hazard for the Tyrnyauz Town (Northern Caucasus, Russia)." In Progress in Landslide Research and Technology, Volume 2 Issue 1, 2023. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-39012-8_10.

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AbstractThe valley of the Gerkhozhan-Su River (a tributary of the Baksan River) in the Norther Caucasus is one of the most debris flow-prone areas in Russia. Large-scale debris flows here have occurred in 1937, 1960, 1961, 1962, 1977, 1999, 2000, 2002, 2011, 2017. The Tyrnyauz town is located in the impact zone of the debris flows. A significant impact on the debris flow hazard in the Gerkhozhan-Su River valley is exerted by the Buzulgan landslide, which was formed on the right side of the valley with a height of about 350 m and an average steepness of 23–25°. The area where the Buzulgan lands

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Ng, Charles W. W., Sunil Poudyal, Haiming Liu, Aastha Bhatta, W. A. Roanga K. De Silva, and Zhenyang Jia. "Investigation of Debris Flow Impact Mechanisms and Designs." In Progress in Landslide Research and Technology. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-44296-4_17.

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AbstractDebris flows are catastrophic landslides increasing in severity in recent decades due to the more frequent and intense rainfall events under climate change. Debris flows pose a serious threat to infrastructure, settlements, and the natural environment in mountainous regions around the world causing considerable economic losses every year. To mitigate debris flows, single and multiple rigid and flexible barriers are constructed along the predicted debris flow paths. Compared with single barriers, multiple barriers are more advantageous in mitigating large debris flow volumes by progress

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Yue, Hai, Dingde Wu, Lifeng Hou, and Mingliang Zhang. "Analysis of the Hydraulic Characteristics of the Debris Flow Disaster Chain in Baozhuping Gully and Analysis of the Conditions for Debris Flow Initiation." In Lecture Notes in Civil Engineering. Springer Nature Singapore, 2024. http://dx.doi.org/10.1007/978-981-97-4355-1_73.

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AbstractTaking the Baozhuping gully landslide-debris flow disaster chain in Ya’an City as an example, through field investigation and on-site measurement, this study analyzed the characteristics of the collapse and breakthrough during the “7.16” debris flow outbreak, and provided the types of dam break and its hydraulic characteristics after the landslide slide. The results show that the instability of the dam body of the pond is mainly due to the damage caused by the overflow of the top, and the maximum flow rate of the dam break reaches 30.12 m3/s, which triggers the initiation of debris flo

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Sodnik, Jošt, Tomaž Podobnikar, Urška Petje, and Matjaž Mikoš. "Topographic Data and Numerical Debris-Flow Modeling." In Landslide Science and Practice. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-31325-7_75.

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Yin, Hsiao-Yuan, and Yi-Min Huang. "TXT-tool 2.886-1.3: Debris Flow Monitoring Guidelines." In Landslide Dynamics: ISDR-ICL Landslide Interactive Teaching Tools. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-57774-6_42.

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Rorem, Erik, Corinna Wendeler, and Andrea Roth. "Flexible Debris Flow Barriers in Fire Burned Areas." In Landslide Science and Practice. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-31337-0_29.

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Huntley, David, Peter Bobrowsky, Roger MacLeod, et al. "IPL Project 202: Landslide Monitoring Best Practices for Climate-Resilient Railway Transportation Corridors in Southwestern British Columbia, Canada." In Progress in Landslide Research and Technology, Volume 1 Issue 1, 2022. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-16898-7_18.

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AbstractThe paper outlines landslide mapping and change-detection monitoring protocols based on the successes of ICL-IPL Project 202 in southwestern British Columbia, Canada. In this region, ice sheets, glaciers, permafrost, rivers and oceans, high relief, and biogeoclimatic characteristics contribute to produce distinctive landslide assemblages. Bedrock and drift-covered slopes along the transportation corridors are prone to mass-wasting when favourable conditions exist. In high-relief mountainous areas, rapidly moving landslides include rock and debris avalanches, rock and debris falls, debr

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Crosta, Giovanni B., and Ko-Fei Liu. "Introduction: Debris Flows." In Landslide Science for a Safer Geoenvironment. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04996-0_1.

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Liu, Ko-Fei, Ting-Iu Kuo, and Shih-Chao Wei. "Debris Flow Detection Using a Video Camera." In Understanding and Reducing Landslide Disaster Risk. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-60311-3_15.

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Wu, Yongqiu, Xilin Liu, Jing’ai Wang, Lianyou Liu, and Peijun Shi. "Landslide and Debris Flow Disasters in China." In Natural Disasters in China. Springer Berlin Heidelberg, 2016. http://dx.doi.org/10.1007/978-3-662-50270-9_3.

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Тези доповідей конференцій з теми "Landslide and debris flow"

Peng, JinCheng, and Guoyue Chen. "Denoising diffusion probabilistic model for accurate super-resolution in landslide and debris flow disaster remote sensing images." In 2024 The 5th Symposium on Pattern Recognition and Applications, edited by Xiaodan Pang. SPIE, 2025. https://doi.org/10.1117/12.3056357.

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Sarafis, I., and J. Zezulak. "Computer analysis of slope failure and landslide processes caused by water." In DEBRIS FLOW 2006. WIT Press, 2006. http://dx.doi.org/10.2495/deb060231.

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Bugnion, L., and C. Wendeler. "Shallow landslide full-scale experiments in combination with testing of a flexible barrier." In DEBRIS FLOW 2010. WIT Press, 2010. http://dx.doi.org/10.2495/deb100141.

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Takaoka, H., H. Hashimoto, S. Ikematsu, and M. Hikida. "Prediction of landslide-induced debris flow hydrograph: the Atsumari debris flow disaster in Japan." In DEBRIS FLOW 2006. WIT Press, 2006. http://dx.doi.org/10.2495/deb060031.

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Brambilla, D., L. Longoni, and M. Papini. "Regional methods for shallow landslide hazard evaluation: a comparison between Italy and Central America." In DEBRIS FLOW 2010. WIT Press, 2010. http://dx.doi.org/10.2495/deb100161.

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Matori, A. N., and A. Basith. "Evaluation of landslide causative factors towards efficient landslide susceptibility modelling in the Cameron Highlands, Malaysia." In DEBRIS FLOWS. WIT Press, 2012. http://dx.doi.org/10.2495/deb120181.

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Riedl, F. J. "Landslide in a catchment area of a torrent and the consequences for the technical mitigation concept." In DEBRIS FLOW 2010. WIT Press, 2010. http://dx.doi.org/10.2495/deb100151.

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Berdos, S., and A. Efremidis. "Evaluating the correlation of extreme climatic phenomena on road slope landslides." In DEBRIS FLOW 2006. WIT Press, 2006. http://dx.doi.org/10.2495/deb060221.

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Zhang, G. P., J. Xu, F. W. Xu, et al. "The triggered mechanism of typhoon-induced debris flows and landslides over mainland China." In DEBRIS FLOW 2010. WIT Press, 2010. http://dx.doi.org/10.2495/deb100061.

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Mrvík, O., and S. Bomont. "Experience with treatment of road structure landslides by innovative methods of deep drainage." In DEBRIS FLOW 2010. WIT Press, 2010. http://dx.doi.org/10.2495/deb100101.

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Звіти організацій з теми "Landslide and debris flow"

Normandeau, A., A. Blais-Stevens, P. Horton, T. Oppikofer, P. Sedore, and V. Maselli. Landslide and debris flows in Pangnirtung Fiord, Nunavut. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329219.

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Huntley, D., D. Rotheram-Clarke, R. Cocking, J. Joseph, and P. Bobrowsky. Current research on slow-moving landslides in the Thompson River valley, British Columbia (IMOU 5170 annual report). Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/331175.

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Interdepartmental Memorandum of Understanding (IMOU) 5170 between Natural Resources Canada (NRCAN), the Geological Survey of Canada (GSC) and Transport Canada Innovation Centre (TC-IC) aims to gain new insight into slow-moving landslides, and the influence of climate change, through testing conventional and emerging monitoring technologies. IMOU 5107 focuses on strategically important sections of the national railway network in the Thompson River valley, British Columbia (BC), and the Assiniboine River valley along the borders of Manitoba (MN) and Saskatchewan (SK). Results of this research ar

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Houck, Karen, Jay Temple, Kassandra Lindsey, Lauren Broes, and Daniel Miggins. OF-20-02 Geologic Map of the Agate Mountain Quadrangle, Park County, Colorado. Colorado Geological Survey, 2024. https://doi.org/10.58783/cgs.of2002.gfnp2602.

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The Agate Mountain quadrangle contains Proterozoic igneous and metamorphic rocks, Paleozoic sedimentary rocks, and Cenozoic volcanic and volcaniclastic rocks. Proterozoic rocks include granite, granitic gneiss, gabbro porphyry, pegmatite, mylonite, and microbreccia. Paleozoic sedimentary rocks include the Manitou Formation, Harding Sandstone, Fremont Formation, Dyer Dolomite, Leadville Limestone, Belden Formation, Minturn Formation, and Maroon Formation. Cenozoic volcanic and volcaniclastic rocks include Wall Mountain Tuff, Thirtynine Mile Andesite, volcanic breccias, trachybasalt, Tallahassee

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Eamer, J. B. R., A. Normandeau, P. Horton, et al. Landslides and debris flows in Grise Fiord, near Ausuittuq, Nunavut. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/331096.

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White, Jonathan, Matthew L. Morgan, and Karen Berry. B-55 The West Salt Creek Landslide: A Catastrophic Rockslide and Rock/Debris Avalanche in Mesa County. Colorado Geological Survey, 2015. http://dx.doi.org/10.58783/cgs.b55.isrw2611.

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Lindsey, Kassandra. Debris Flow Susceptibility Map for Mount Rainier, Washington Based on Debris Flow Initiation Zone Characteristics from the November, 2006 Climate Event in the Cascade Mountains. Portland State University Library, 2000. http://dx.doi.org/10.15760/etd.2650.

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Tao, Liu, McGuire Luke, Youberg Ann, et al. A prefire approach for probabilistic assessments of postfire debris-flow inundation. Office of Scientific and Technical Information (OSTI), 2024. http://dx.doi.org/10.2172/2373168.

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Yu, Hsu-Chun James, Zhong-Hung Lee, Cai-Fang Ye, Lan-kun CHUNG, Yao-Min Fang, and Jen-Chu Liu, eds. Sensor Web Enablement Application for Debris Flow Monitoring System in Taiwan. Open Geospatial Consortium, Inc., 2009. http://dx.doi.org/10.62973/09-082.

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Luternauer, J. L., and K. W. Conway. Extensive postglacial debris flow on the Central Continental Shelf of British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130068.

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Jochim, Candace L. SP-30 Debris-Flow Hazard in the Immediate Vicinity of Ouray, Colorado. Colorado Geological Survey, 1986. http://dx.doi.org/10.58783/cgs.sp30.qqti2400.

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