The terrain, ie. the form of ridges and valleys, can be a reasonable indicator of rock fracturing, including the direction and extent of fracturing. This digital elevation map (DEM) can also be used to define the direction of the surficial drainage system (eg. creeks and rivers), catchment boundaries slope and aspect.

Gravity is the force of attraction between masses. The airborne gravity data used in this image are coarse, however the data provides another level of discrimination for the location of deep groundwater sources. The areas of most interest are the low magnetic values (blue) which can be indicators of deep groundwater basins, sinks or confined groundwater sources.

The airborne magnetics provide the variation in magnetic emissions from the Earth. Magnetic images in this report have high magnetic susceptibility as red and low susceptibility as deep blue patterns. The deep blue represents potential groundwater sources or highly weathered rock materials. These images provide the best indicator of deep groundwater resources within this overall data set.

The radiometrics are derived from airborne gamma-ray data emissions that are the breakdown of radionuclides, such as Uranium, Thorium and Potassium. The Uranium radionuclide is the source of radon gas that can be high on granite soils and in saline pathways. Radon hotspots are in red. The radiometrics (as a total count of gamma-ray) are used to define shallow water sources or saturated soils that are often associated with low gamma-ray emissions, as seen by the deep blue in the above image.

This radiometric composite image highlights the variation between Uranium (purple and bright yellow), Thorium (greenish yellow) and Potassium (black).

The geology of an area provides a fundamental base for assessment of the rock system, the nature of the rock type (eg. igneous, sedimentary, or metamorphic) and the extent of rock deformation or fracturing. Geology has both spatial and time dimensions that form the dynamics or complexity of the groundwater assessment.

The aerial photo provides the fine resolution of land use, infrastructure (eg. buildings, dams, fence lines, trees, and roads/tracks) that are necessary for field navigation to selected bore hole sites.

The satellite data are included to provide the land cover types (eg. vegetation, crop, etc.) in the study area differences.

This data set is a composite of gravity and magnetic data that are classified to determine spatial patterns that represent the correlations (spectral and spatial), highlighting potential areas for deep groundwater exploration at local scales.

The radiometric classification of the total count (TC) provides fine details of the soil property differences, salinity pathways, surficial rock structures, and generally is a good guide to shallow groundwater expressions or buried paleochannels.