Photography Circus of Pougnadoires Bra Of Tarn Towards 1920

Description

ph32
Dimensions
: 10.5cm by 4.5cm
Glass stereoscopic plate
e
.
Quick and neat delivery .
The gorges are dug in secondary limestones which start from the Bajocian at the base (dolomitic bars), continue through the lower Bathonian above, characterized by an inclined slope, and finally end in large vertical cliffs (Bathonian dolomite and Upper Jurassic dolomite). This relatively simple architecture characterizes the downstream part of the gorges (between Les Vignes and Le Rozier) but upstream, the presence of faults (Hauterive fault, Ste Enimie submeridian accident which also crosses the entire Causse Méjean) makes the geology there more complex. It is these faults which are precisely at the origin of two exsurgences with a very high flow in the region of Ste Enimie: the source of Burle and the source of Coussac, the latter falling
Dimensions : 10.5cm by 4.5cm Glass stereoscopic platee . The gorges are dug in secondary limestones which start from the Bajocian at the base (dolomitic bars), continue through the lower Bathonian above, characterized by an inclined slope, and finally end in large vertical cliffs (Bathonian dolomite and Upper Jurassic dolomite). This relatively simple architecture characterizes the downstream part of the gorges (between Les Vignes and Le Rozier) but upstream, the presence of faults (Hauterive fault, Ste Enimie submeridian accident which also crosses the entire Causse Méjean) makes the geology there more complex. It is these faults which are precisely at the origin of two exsurgences with a very high flow in the region of Ste Enimie: the source of Burle and the source of Coussac, the latter