This map is a layout of the KGS Geologic Map Information Service which activates layers that display the locations of known landslides and areas susceptible to landslides in a geologic and geomorphic context. The purpose of the map is to provide an overall view of landslide hazards across the state. Locations come from Kentucky Geological Survey research, published maps, state and local government agencies, the public, and media reports, thus making attributes and spatial accuracy highly variable. This map can be used to identify preexisting landslides and serve as a basis for landslide hazard and risk assessments. It is not intended for site specific investigations. The absence of landslides in an area does not infer that a landslide does not exist or that the ground is stable. A professional geologist or geotechnical engineer should be consulted for planned construction at identified landslide locations or identified landslide areas. A professional geologist or geotechnical engineer should also be consulted for slope stabilization and other mitigation efforts related to existing slides.
The default Base Layer shown is a LiDAR-derived multi-directional hillshade (1.5 m). The LiDAR layer (Layers menu - under the "KYFromAbove Layers" heading) can be adjusted for varying amounts of transparency and is particularly useful to view with the geology layers and/or the aerial photography Base Layer. There are five landslide data layers represented as either points, lines, or polygons.
Landslide Map Layer Descriptions
Five layers are contained within the "KGS Landslide Data" layout. Their descriptions are as follows:
KGS landslide inventory data
This map layer contains known landslide locations (points) across Kentucky compiled in a landslide inventory database. The locations come from Kentucky Geological Survey research, state and local government agencies, and the public. Many of the points represent larger landslide features that have not been mapped in detail and may fall within different parts of the slide area (crown, head scarp, middle, or toe). The landslides are active or have historically been active. Slide locations are collected at different times and contain varying amounts of attributes. The inventory does not capture work by private industry or other agencies that document landslides but do not make them available. Many attribute values are "Null" and data is only present if the slide was visited or could be collected another way. Landslide inventory points that fall within a landslide polygon layer represent the centroid of that polygon so it could be catalogued in the inventory database.
The SourceDesc field describes the source of the landslide location. KGS=Kentucky Geological Survey, KY EM = Kentucky Emergency Management, KYTC = Kentucky Transportation Cabinet, DNR-DMRE = Division of Natural Resources-Mine Reclamation & Enforcement, NRCS = Natural Resource Conservation Service, NKAPC = Northern Kentucky Area Planning Commission, NKU = Northern Kentucky University.
1:24,000 geologic map landslides
These landslide locations (polygons) were mapped on 7.5-minute, 1:24,000-scale geologic quadrangles published jointly by the Kentucky Geological Survey and US Geological Survey from 1960 to 1978. Attributes include original map symbol and formation name, as well as county, quadrangle, and Area Development District. Landslides were not mapped on all quadrangles. Search source data on the KGS publications search page.
Derived from LiDAR
These landslides (polygons) were interpreted and mapped using LiDAR-derived digital elevation models (DEM) that range from 1 to 1.5-meter horizontal resolution and have a quality level of 1 to 3. The quality level refers to nominal pulse spacing (NPS), which is an aggregate of all strikes and is approximately < 0.35 to < 1.4 m). Ground strike spacing, which is what is used to generate bare earth hillshade models, will typically be greater that the aggregate NPS. Primarily using LiDAR-derived hillshades, potential landslide extents were identified and digitized. Extents of landslides that included features such as headscarps, flanks, toe slopes, and hummocky topography were digitized as GIS polygons. Secondary support maps of slope, roughness, curvature, plan curvature, and contours, as well as aerial photography, were used to help identify landslide features and constrain confidence in interpreting landslide extents. Locations were field verified, where possible. Comments included are notes and observations taken during the mapping of these slides. For information regarding LiDAR acquisition visit KY From Above
For more specific information regarding mapping these landslides see:
Derived from Aerial Photos
This layer (polygons) represents mapped landslides including earthflows, debris slides, and slumps. The data come from a series of published Landslide and Related Features Maps and Landslide Potential Maps that cover most of southeastern and south-central Kentucky. Landslides were interpreted from aerial photographs and historical records. The features digitized (polygons) depict generalized slope conditions as they existed at the time of field checking (1977-1981). Slope stability may decrease by excavation, loading, and changes in drainage conditions. The data are from preliminary type maps and are suited for general planning purposes only. Search source data on the KGS publications search page.
Areas susceptible to debris flows
This layer (lines) represents debris flow deposits or areas susceptible to debris flows. Primarily these areas are shallow, narrow ravines containing variable accumulations of hillslope soil called colluvium. The data come from a series of published Landslide and Related Features Maps and Landslide Potential Maps that cover most of southeastern and south-central Kentucky. The features were interpreted from aerial photographs and historical records. The debris flows digitized (lines) depict generalized slope conditions as they existed at the time of field checking (1977-1981). Areas of thick colluvium are susceptible to rapid movement during intense rainfall. The data are from preliminary type maps and are suited for general planning purposes only. Search source data on the KGS publications search page.
A semi-quantitative confidence ranking is assigned to each landslide feature. Based on Mirus and others (2020), confidence rankings range from “1” (low confidence) through “8” (high confidence) and reflect the relative value of different data.
8 – High confidence that the nature and/or spatial extent of the landslide is well characterized
This highest confidence level is typically based on detailed field observations and/or expert
analysis of high-resolution topographic data or aerial imagery to characterize the landslide.
5 – Confident that a consequential landslide took place at the specified location
This level of characterization still involves high confidence that a landslide took place at
the specified location as evidenced by fatalities and/or damage to infrastructure, but
detailed observations of landslide features are not described in the geodatabase.
3 - Landslide likely at or near the specified location
This middle confidence level reflects a known landslide occurred with lower certainty on
the exact position or nature of the slope failure. These typically include verified landslides
on lower resolution topographic maps or aerial imagery and landslide data that predates
digital topography and precise global positioning systems
2 - Probable landslide in the area
Although the exact location and extent of the landslide is not documented, it is probable
that a landslide did occur within close proximity to the specified location. This includes
geologic mapping of landslide deposits that may correspond to multiple landslides as well
as individual landslides mapped with low resolution topographic data.
1 - Possible landslide occurred in the area
The lowest confidence level reflects the uncertain nature of some media reports and the
lack of expert classification and characterization from old maps.
Landslides are the downslope movement of rock, soil, or both under the influence of gravity. A combination of steep slopes, excessive pore-water pressure, weak rocks and soil, and slope modification commonly contributes to landslide occurrence. Landslides types vary by the rate of movement, style of movement, and type of hillslope material involved (Figure 1).
Landslides are caused by stresses on a slope that exceed the strength of the hillslope soil. Stresses can include increased pore-water pressure (from rainfall), gravity, or some type of slope modification (loading or excavating). Intense or long-duration rainfall can trigger slides, rock falls, debris flows, or other landslide types. The danger is greatest during the late winter and early spring months, before large trees leaf out and remove water by evapotranspiration as it infiltrates into hillside soils. These stresses act over time and space at different scales and magnitudes, often making hazard and risk assessment challenging. Diverse terminology and definitions among geologists, engineers, and the public are a reflection of the complex landslide processes. Some of the most common terms are landslide, mudslide, and rockslide. Other terms such as mass wasting, slope movement, and slope failure are also commonly used to discuss landslide phenomena. Regardless of which term is used, all landslides share physical and mechanical (in rock and soil) processes that explain their occurrence.