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Transhumance in Alpes-de-Haute-Provence, France. Transhumance is a type of pastoralism or nomadism, a seasonal movement of livestock between fixed summer and winter pastures. In montane regions (vertical transhumance), it implies movement between higher pastures in summer and lower valleys in winter. Herders have a permanent home, typically in ...
Transhumance is an ancient Italian custom, by which large flocks of sheep in the mid fall were driven south from the hilly and mountainous regions of the Apennines to winter over in the more southern coastal plains of Apulia and, less commonly, Lazio.
As transhumance takes place in summer, during school holidays, the transhumance does not affect schooling. Young herders take their text books of the upcoming school year to the grazing grounds. Among the popular games on the grasslands, football (introduced via schools) tends to replace the traditional ‘’ qarsa ’’ game.
Alpine transhumance is transhumance as practiced in the Alps, that is, a seasonal droving of grazing livestock between the valleys in winter and the high mountain pastures in summer (German Alpwirtschaft, Almwirtschaft from the term for "seasonal mountain pasture", Alp, Alm). Transhumance is a traditional practice that has shaped much of the ...
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Land of pastoral tradition and marked by transhumance, currently herds of ovejas merinos continue to go up to the ports of Babia, which are leased for the entire season and share the pastures with cattle and, also with the equine, especially of the Hispano-Breton breed, Babia being the state reference for this horse.
For Kfarsghab, the seasonal transhumance is still respected as agriculture remains the main activity. [ 16 ] Kfarsghab , the summer village, is located on the road going from Ehden to Bsharri in the northern part of the Qadisha valley, overlooking the Qozhaya valley at an average altitude of 1380 meters.
[8] Three periods of magmatic activity (volcanic action) have been identified, 147–106 Ma, 97–81 Ma and 68–49 Ma. The first is prominent in the north of the trough, and contemporary with magmatism in Brazil, probably occurring during a period of crustal extension before the Atlantic started to open. The second is found only in the south ...