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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

Application of principal component analysis to geo-electrical recordings

TL;DR: In this article, the use of the well-known method, i.e., principal component analysis (PCA) as a filtering tool is tested on the geoelectrical time series acquired in the Mt. Vesuvius area (Naples, Italy).
Journal ArticleDOI

The Electrical Resistivity Tomography Technique for Landslide Characterization in Blangkejeren Aceh

Abstract: Investigation of geophysical methods describes elements and geological geometry based on the physical properties of the subsurface. In the past decade, the application of resistivity methods has experienced a rapid increase in describing geological structures and settings. The Electrical Resistivity Tomography technique used to describe the geometry of a complex landslide in Blangkejeren, Aceh province, Indonesia. This area is highly influenced by the landscape with slopes, high-rainfall, and tectonic activity of the Sumatran fault which can lead to soil movement. The type of landslides in this area is largely controlled by geo-structural characteristics; rotational and translational slides, as well as the phenomenon of the gravitational slope of high steepness. As a preliminary study, the acquisition of resistivity data was conducted at two locations with a length of each measuring path 330 meters and electrodes spacing 6 meters. The Supersting R8/IP instrument unit with Wenner-Schlumberger array is used to obtain data that has a sensitivity to vertical and lateral changes. The resistivity distribution along the path is obtained from both profiles that are perpendicular to the landslide field. ERT modeling results at both locations showed subsurface structures based on resistivity values such as; slate, clay, and sandy clay. The contrast resistivity between each layer makes it easier to describe the characteristics of the landslide slip plane geometry which is affected by the slope angle. The resistivity method has physical properties that are very sensitive to porosity and groundwater which is the main parameter in a landslide. Finally, it should be noted that the use of the ERT technique as an effective and efficient method in conducting landslide studies as a disaster mitigation effort.
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Ground and Satellite-Based Methods of Measuring Deformation at a UK Landslide Observatory: Comparison and Integration

TL;DR: In this article , the authors presented a case study of the Hollin Hill landslide in North Yorkshire where a variety of ground-based geophysical measurements are available for comparison with InSAR data.
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Spontaneous Potential investigations in Semenic Mountains

TL;DR: In this paper, a series of mesh grids have been made in areas with different characteristics (lithology, pedology, slope, exposition, etc.) at different time periods in order to spot and analyse the change in data in the chosen sites, various conditions given.

Vadose Zone Thickness Limits Pore‐Fluid Pressure Rise in a Large, Slow‐Moving Earthflow

TL;DR: In this article , the authors exploit a multi-year record of precipitation, pore pressure, and velocity from Oak Ridge earthflow, a slow-moving landslide set in Franciscan mélange, northern California, USA.
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.
Journal ArticleDOI

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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