Hitting bedrock
One of the farmers we worked with kindly supplied us with a sample of the bedrock from their farm. We carried out
compositional analysis
, explored scientific literature, and delved into the geological maps of the local area to establish the history of the bedrock.
In this case, we were able to identify the bedrock as a Devonian mudstone and shale, some 420-320 million years old. This element map shows the distribution of different minerals in the sample, including quartz, muscovite mica, biotite mice, chlorite, and a rare earth element-bearing mineral that was likely weathered out from the nearby Dartmoor granites. This bedrock weathers into soil, so these minerals were also identified in the soil itself.