Ann: Pensana granted major new rare earth exploration project, page-6

Having now read the Paper that this came from I would like to point out that it is an Academic publication and as such fails to pursue the economic potentials. To be fair to the authors they do point out their inability to access and test the central core due to soil cover.

The distribution in concentric rims of these magmatic breccia outcrops suggests that
the structure of Monte Verde could correspond to the inner part of a collapsed caldera, and the
breccias could represent channels (ring-faults) of extrusion controlled by subvolcanic explosive
processes. A similar mechanism was proposed for Alnö [60] to explain the existence of carbonatite
ring dykes in Sweden. Hence, by assuming that the structure could correspond to a partially eroded
caldera structure, the area with carbonatite potential should be expanded, and the potential for larger
intrusions at depth would still persist. In fact, colluvial materials cover large areas around the core of
the complex, and therefore, more distal hidden carbonatite rings could also be present beneath these
colluvial sediments.

It certainly sounds like another Longonjo, I just hope that the soil cover is not too deep,
A quick GPR study, followed up by a couple of drill holes will soon reveal what is underneath