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Three-dimensional geophysical anatomy of an active landslide in Lias Group mudrocks, Cleveland Basin, UK

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TLDR
In this article, a geoelectrical investigation of a slow moving earth slide in Lower Jurassic Lias Group rocks of the Cleveland Basin, UK, is described, which includes a reconnaissance survey phase using two-dimensional electrical resistivity tomography (ERT), resistivity mapping, self-potential (SP) profiling and mapping, followed by a detailed investigation of an area of the landslide using three-dimensional (3D) ERT and selfpotential tomography.
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This article is published in Geomorphology.The article was published on 2011-02-15 and is currently open access. It has received 145 citations till now. The article focuses on the topics: Landslide & Electrical resistivity tomography.

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Journal ArticleDOI

Four-dimensional imaging of moisture dynamics during landslide reactivation

TL;DR: In this article, a 3D time-lapse resistivity imaging on an active landslide was used to provide long-term data highlighting the evolution of moisture content prior to landslide reactivation and showing its decline post reactivation.
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UAV monitoring and documentation of a large landslide

TL;DR: In this paper, a bundle of technologies was applied to monitor and document the landslide, such as geophysical methods (geoelectrics, inclinometer, soil moisture, and soil temperature) and Global Navigation Satellite System (GNSS) measurements.
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A Review of the Advantages and Limitations of Geophysical Investigations in Landslide Studies

TL;DR: In this paper, the authors focused on works of the last twelve years (2007-2018), and the main goal is to analyse the geophysical community efforts toward overcoming the geophysics and landslide review highlighted in the 2007 geophysicists and landslides review.
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Bedrock detection beneath river terrace deposits using three-dimensional electrical resistivity tomography

TL;DR: In this article, a 3D electrical resistivity (3D ERT) was used to identify the steepest gradient in first-derivative resistivity profiles, which yields an estimate of bedrock depth (verified by drilling) to a precision better than 0.2m.
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Evolution of soil wetting patterns preceding a hydrologically induced landslide inferred from electrical resistivity survey and point measurements of volumetric water content and pore water pressure

TL;DR: In this article, electrical resistivity tomography (ERT) was used to monitor the hydrological state of a hillside prior to a sprinkling-induced shallow landslide, and the results indicate that when large and interconnected regions of hillslope are saturated (as confirmed by high volumetric water content and low standard deviation of water saturation), additional water cannot be redistributed to empty drier regions and may eventually enhance local pore water pressure and seepage force, initiating large shear deformation and failure.
References
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Journal Article

Landslide types and processes

TL;DR: In this paper, the authors reviewed the range of Earth surface movements that may be classified as LANDSLIDES and classified them according to the following: Falling, sliding, or flowing.
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Electrical resistivity survey in soil science: a review .

TL;DR: In this paper, the authors overview the variation of electrical resistivity as a function of soil properties, and the main electrical device to performed one-, two-or three-dimensional surveys, and explain the basic principles of the data interpretation.
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A numerical comparison of 2D resistivity imaging with 10 electrode arrays

TL;DR: In this article, numerical simulations are used to compare the resolution and efficiency of 2D resistivity imaging surveys for 10 electrode arrays, including pole-pole (PP), pole-dipole (PD), half-Wenner (HW), Wenner-α (WN), Schlumberger (SC), dipole-dipsole (DD), WenNER-β (WB), γ -array (GM), multiple or moving gradient array (GD) and midpoint-potential-referred measurement (MPR) arrays.
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