Services
GPR is reliable way of detecting geological features and deep layers.
Ground
Penetrating Radar (GPR) can be used for geological surveys to detect features
such as the bedrock, water table, and stratigraphic layers. GPR can also be
used to measure the thickness of ice sheets, and the profile of river or canal
beds with some penetration into the soil beneath – which is not possible using
only a sonar-based system.
For the
detection of the bedrock, water table and the stratification of the ground, the
use of a very low frequency antenna is required. This could be anything between
25MHz and 100MHz. In the right conditions such GPR have penetration into the
tens of meters. Such GPR have very poor surface resolution and are of little
use for typical applications, but they can detect very large features and
interfaces (layers) which are located deeper in the ground.
Benefits of using GPR surveys to detect deep layers
Why choose us for geological GPR survey
 |
Our surveyors have used all types of low frequency GPR |
|
Experienced surveyors have worked in multiple locations |
|
Detailed drawings and clearly presented results |
|
GPR and Geophysical survey experts |
Our other offer
FAQ
What are stratigraphic layers?
Deep stratigraphic or geological layers are the successive, horizontal layers of rock, sediment, or soil that have accumulated over geological time, providing a record of Earth's history and past environmental conditions.
Why detect bedrock using GPR?
Detecting bedrock is essential for understanding the geological foundation, ensuring the stability and suitability of construction projects, and providing critical information for resource extraction and environmental studies.
Contact us
