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Its territory ranges from 50 to 600 ha it marks with its droppings and urine or se-cretion of the glands between the toes of his feet These olfactory in addition to informing its congeners in its home range facilitate the orientation of the fox that is-sued overnight This scent marking is placed visibly in the territory

PDF HANDMADE TERRITORY: CRAFTS AS IDENTITY EXPRESSION IN

HANDMADE TERRITORY: CRAFTS AS IDENTITY EXPRESSION IN REMAINING QUILOMBOLA COMMUNITIES 1 Universidade Federal de Santa Maria 2 Universidade Federal de Santa Maria 74

  • What do handmade items tell us?

    Handcrafted items can tell us about the stories behind them; from their design to the materials used in production, each item has a unique story that contributes to our understanding of certain cultures or regions. By looking at handmade crafts from around the world, we gain insight into how other societies live and what they consider important.

  • What are handmade crafts?

    These works of art often represent traditional values, beliefs and techniques passed down through generations. Handmade crafts can range from pottery to intricate jewelry, clothing to furniture – all crafted with skill and love. Exploring the handmade crafts from around the world offers an opportunity to gain insight into different cultures.

  • How have handmade crafts impacted globalization?

    Handmade crafts from around the world have been an important part of many cultures for centuries. They can be seen as expressions of identity, and for many people, a way to pass on their traditions. In this article, we will explore the impact these handmade crafts have had on globalization.

  • How can handmade crafts help you explore different cultures?

    The world is filled with an abundance of cultures, all unique and fascinating in their own ways. One way to explore these different cultures is through handmade crafts, which have been used for centuries as a form of communication and storytelling.

Sidi Boulknadel Pipes

The Sidi Boulknadel pipes dissolution exists in a quarry located about 30 km north of Rabat (Fig. 3). It is bordered to the North by the Plage des Nations, to the South by the exotic garden, to the East by the Maamora forest, and to the West by the Atlantic Ocean. This quaternary aged quarry is open in an internal coastal barrier located at the eas

Carboniferous Hills of Korifla River Panorama

This site is located 40 km from Rabat (Fig. 4a). The hills are composed of sandstone-pelitic formations organized in flysch with turbiditic characteristics attributed to the Upper Visean (Termier 1936; Piqué 1979). These geological and educational outcrops make it possible to show and illustrate the traces of the Hercynian deformation (Fig. 4b and

Lower Devonian Carbonate Concretion East of Ezzehiliga

East of Ezzehiliga, a small quarry is open on the side of the road; this quarry presents a series made up of clays; it is a black flaky pelite due to the presence of organic matter rich in graptolite fossils that allow this deposit to be dated from the Silurian and early Devonian, then a series of basal limestones from the Lower Devonian marked by

Normal Fault of El Malha River

Toward the south of the rommani inlier, a few tens of meters before the bridge which crosses the El Malha River, a formation of three shades of rocks which follow one another in a few meters (Fig. 6). A brown rock with a flaky appearance, it is an alternation of strata, some harder than sandstone and others much less resistant to erosion, made up o

Pillow Lava of Malha Valley

Toward the south of the Rommani inlier, there are pillow lavas shaped in onion peels (Fig. 7a and b), which are well-preserved magmatic rocks from the Triassic period of Morocco, hence their interest as a geological heritage. This onion peel basalt structure results from a meteoritic weathering process rich in silica with the presence of quartz and

Volcanic Flow of Boulhmayl River

Near the Boulhmayl River, at the bend of the road that winds between Oulmes and Khenifra, there is a cliff overlooking the road (Fig. 8). This cliff is a splendid natural site and a scenario of installation it is about a plio-Quaternary volcanic flow. It allows us to retrace its history. At the beginning of this period, the Oued boulhmayl has just

Gayville Beach Potholes

In Gayville beach there are potholes in a calcarenite made up of well classified medium to coarse sands (Fig. 9). The process of formation of potholes is the dissolution and eddy current, and associated with mechanical erosion of sea water, and rain becomes loaded with carbon dioxide. The dissolution of limestone is possible when there is presence

Koudiat Ech-Cherif

The carbonates of Koudiat Ech-Cherif, from the lower and middle Devonian form a large mass surrounded by the facies of the Famenno-Tournaisian. This carbonate mass is in the form of a flap 5.5 km in length, of variable thickness, and surrounded by the facies of the formation of Fouizir. Its northern limit is marked by an accident, showing a late ga

Sebt-Merchouch Plateau Angular Unconformity

Forty kilometers from Rabat, in the direction of Merchouch, the road begins to descend into the valley of the Oued Korifla, which makes it possible to cut the rocks forming the Sebt Merchouch plateau and to access the deeper rocks and the angular unconformity (Fig. 11) between the Miocene and the Carboniferous (Middle and Upper Visean) is a good ex

Zaër Granite

The granitic pluton of Zaër outcrops (Fig. 12) in the north-western part of central Morocco is in the shape of an ellipse, about 40 km long and 15 to 20 km wide, oriented NE-SW parallel to the major regional structure (Michard 1976; Piqué 1994). It represents the largest granite massif of the Hercynian range of Morocco, whose radiometric ages from

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