Photography Circus of Pougnadoires Bra Of Tarn Towards 1920
The description of this item has been automatically translated. If you have any questions, please feel free to contact us.
ph32
Dimensions :10.5 cm by 4.5 cm
Stereoscopic glass platee .
Quick and neat delivery .
The gorges are dug in secondary limestones which start from the Bajocian at the base (dolomitic bars), continue with the lower Bathonian above, characterized by an inclined slope, and finally end with large vertical cliffs (Batonian dolomite and Upper Jurassic dolomite). This relatively simple architecture characterizes the downstream part of the gorges (between the Vignes and the Rozier) but as far as the upstream is concerned, the presence of faults (Hauterive fault, submeridian accident of Ste Enimie which also crosses the entire Causse Méjean) makes the geology more complex. It is these faults which are precisely at the origin of two e
Dimensions :10.5 cm by 4.5 cm
Quick and neat delivery .
The gorges are dug in secondary limestones which start from the Bajocian at the base (dolomitic bars), continue with the lower Bathonian above, characterized by an inclined slope, and finally end with large vertical cliffs (Batonian dolomite and Upper Jurassic dolomite). This relatively simple architecture characterizes the downstream part of the gorges (between the Vignes and the Rozier) but as far as the upstream is concerned, the presence of faults (Hauterive fault, submeridian accident of Ste Enimie which also crosses the entire Causse Méjean) makes the geology more complex. It is these faults which are precisely at the origin of two e