Anti atlas

The Anti Atlas is a little-known Moroccan mountain. Discovery of a rich heritage * of André Humbert & Herbert Popp. The Anti Atlas is a chain of mountains in the southwest of Morocco, oriented southwest and northeast over nearly 600 km, located between the central High Atlas and Souss au Tafilalet.

 

Trekking in Morocco, Toubkal Ascent

Mount Toubkal Adventures Mount Toubkal: The Toubkal massif is made up of rocks of various kinds. We find in particular on the summits of andesite and rhyolite, dark rocks of volcanic origin. Glaciers have left characteristic marks of their passage in the form of trough valleys. During the Würm glaciation, the current valley of Assif n’Ait Mizane (the valley of the Toubkal refuge) was occupied by the longest glacier in the Atlas. It was 5 km long. The word Toubkal would be a deformation of French origin of the same Berber name Tugg Akal /toug-akal/ which means “she who looks up at the earth” Where is Mount Toubkal? One of the most beautiful mountains of the High Atlas Mountains chain, which passes in the countries of the Maghreb, as Mount Toubkal or Mount Toubkal is the highest mountain peak in the Atlas Mountains chain, which has a height of 4165 meters and is 60 km south of Marrakesh.  It has two types of slopes, The first is the high slopes to which most people tend to practice climbing, which are covered with snow in the winter season, so people practice skiing, and the second is the low or lower slopes, which individuals go to for recreation and enjoying the scenery, you will need two full days to reach the top of a mountain Toubkal and the landing thereof. On the first day, you will leave from the village of Imlil in the morning and walk for about five hours to the shelter, where you will spend the night. Then on the second day you will go to the summit in a period of four to five hours, then head down to the shelter, then return to Imlil, the best period to climb Mount Toubkal is late April to October and great care must be taken when climbing the mountain. Mount Toubkal featured treks: Toubkal Ascent 2 Days: Day 01: Transfer by Minibus to the High Atlas/Imlil village 1800m/Refuge Toubkal (3200m). At 8am our taxi or minibus driver (minibus for more than 4 participants) will pick you up at your hotel or fix the starting point in advance, example Jammaa El fena place near Café FRANCE, drive towards Toubkal, 1h 30 by car from Marrakech to reach the village of Imlil starting point of your hike, in the village you will meet our local team, guide and muleteer, start of trek to the refuge of Toubkal? crossing of Village Armed then we continue along the assif Ait Mizan to reach the marabout of Sidi Chamharouch, place of lunch, in the afternoon a climb of 400 m to reach the refuge of Toubkal, night at the bivouac or refuge (refuge in winter, bivouac in summer). Elevation M: 1450 m Elevation D: 30 m Walking time: 6 hours Accommodation: in a tent or refuge. Day 02: Toubkal Refuge – Ascent of Mt Toubkal – Armed 1900m Departure early in the morning for the ascent of Mount Toubkal, the highest in North Africa, is done without difficulty, after 2 hours of climbing we will reach a pass at 3900m which covers the Siroua massif and the hamadas of southern Morocco, we continue successively towards the geodesic point 4167m. very wide 360 ° view on all directions: valleys, surrounding peaks, the Anti Atlas, the pre-Saharan mountains and the plain of Marrakech. Descent by the same path, continuation along the Assif Ait Mizane, lunch and visit of marabout Sidi Chamharouch, place of pilgrimage, to reach the village of Armed where we will find our car, return to Marrakech. Toubkal Climb 3 days Itinerary Day per Day: Day1: Marrakech – Imlil After arrival in Marrakech, you wil be transferred to the little village of Imlil. Here you will be able to explore the area and you will spend the night in a guesthouse. Day 2: Imlil – Toubkal Refuge Today we begin our trek. Heading along the Ait Mizane Valley, we first past the village of Aremd and then into the shrine of Sidi Chamarouch. We then continue east and by crossing the flood plains our route takes us along mule tracks and up into the high rocky cliffs above the valley. Crossing the river we eventually come to the pastoral shrine of Sidi Chamarouch, which attracts tourists and pilgrims. From here the trail continues to climb steadily, snaking and zigzagging its way up to the snowline and the Toukbal Refuge (3206m), our stop for the night.  Approx: 4 to 5hrs walking. Day 3: Toubkal Refuge – Summit – Refuge – Imlil – Marrakech Early in the morning we make our attempt on the summit of Jebel Toukbal, the highest peak in Northern Africa. Our route takes us up the south cirque, crossing the stream above the refuge. The walking is relatively straightforward, but the ice and the altitude will make the going quite difficult in parts. The views along the way make the journey more than worthwhile. When you reach the summit you will see that the vistas across the surrounding landscape are quite breathtaking. From here there are unrestricted views in every direction, from the Marrakesh Plain to the High Atlas in the north and as far south as the Anti-Atlas and the Sahara. We will retrace our steps when we return down the mountain and head back towards Imlil. Transfer back to Marrakech. Approx. 9hrs walking.   Toubkal National Park summer Trek 8 days From the Atlas to the heart of the medina of Marrakech, this Moroccan adventure offers us an astonishing combination of sporting challenge, magical encounters and spectacular landscapes. We will experience the hospitality of the Berber people in the High Atlas region where the highest peaks are located, including Toubkal at 4,167 m … From the top, the reward is fantastic: a panorama over the whole region. Day 1:Marrakech – Imlil (1750m) – Camp of Toubkal (3200m) Transfer to Imlil, from where we will start our trek. We will first cross magnificent gardens and apple and walnut orchards to arrive

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GEOLOGY OF THE SURROUNDINGS OF MARRAKECH

GEOLOGY OF THE SURROUNDINGS OF MARRAKECH

GEOLOGY OF THE SURROUNDINGS OF MARRAKECH Mount Toubkal: GEOLOGY OF THE SURROUNDINGS OF MARRAKECH On a local geological map we see 3 main groups: The Haouz The High Atlas of Marrakech The Jebilets The city of Marrakech is built on a large sloping surface from the feet of the High Atlas in the south to the valley of the Wadi Tensift: the plain, or rather the piedmont, of Haouz. To the north extend the peeled hills of Jebilets crossed by the road to Casablanca. The Haouz plain is made up of the products of the erosion of the High Atlas mountains by torrents. These torrential alluviums are made up of gravel and gravel and silt, particularly suitable for the cultivation of fruit trees. The Jebilet are mainly made up of old detrital sediments deposited in the primary era, then folded and faulted and recrystallized, predominantly gray to yellowish in color. They represent the heavily eroded remains of an ancient mountain range. The High Atlas of Marrakech is a young mountain range, contemporary with the Alps in Europe. It consists of sedimentary rocks of reddish color (sandstone, sandstone clays) or yellowish-white (limestone) mainly deposited in the marine environment during the secondary era and which were folded and fractured during the tertiary era. These rocks are based on an older set of rather grayish to yellowish color, which was folded and fractured during the primary era like the Jebilet. This “Hercynian base” outcrops in the center of the chain, as in Tizi n’Tichka, Jebel Toubkal, it includes grayish schists and in particular granites. Elements of geology for tourists in a hurry The geology of the Marrakech region provides a good illustration of continental drift (plate tectonics) which can be summarized as follows: – the continental masses move away (extension): the liberated spaces fill with marine sediments – the continental masses approach and collide (convergence and compression): the sediments fold, fracture, and form a mountain chain. In the Marrakech region, the first well-known mountain range was formed during the Precambrian era, around 1 billion years ago. It was eroded during a large part of the primary era during a period of extension and provided the materials for marine sediments of the primary era, here especially detrital sediments (pebbles, sands, etc.)At the end of the primary era, the continental masses approach, and the sediments are deformed and build a new mountain chain, the Hercynian chain, in Europe and Morocco. Its remains are still clearly visible in the Jebilet massif and in the axis of the High Atlas of Marrakech. Primary lands deformed by the Hercynian orogeny: 1. Sandstone and primary folded schites   2. Flaw in a pleated ensemble. In turn, the latter is eroded during the extension period of the secondary era; marine spaces are filled with debris (detrital sediments) and limestone rocks produced by the activity of living marine beings (corals). Extension fractures allow volcanic products to rise (basalt flows). The red layers of the Permo-Triassic: 3 and 4. the “Grés de l’Oukaïmeden” 5. Fine clayey sandstone (siltstone) and sandstone 6. sloping surface of the Oukaïmeden sandstone, red siltstones, and gray basalt flow. Finally, the convergence of the continents during the tertiary era produced the uplifting of the alpine chain which extends over Europe and North Africa and of which the High Atlas of Marrakech is a part. The current Quaternary era is again a period of calm with the erosion of the reliefs and accumulation of detrital at their feet and beyond. Road routes The 3 roads which from Marrakech enter the High Atlas provide a good example of the different rocks constituting the High Atlas. 1.Ourika Valley, Oukaimeden: the red rocks of the Permo-Triassic (end of Primary-beginning of Secondary) are dominant. The sandstones from cliffs. Above the fine clayey sandstones (siltstones) lie flows of altered yellowish-gray basaltic lava. 2. Tizi n’Tichka road: it crosses the red layers, basalts, and very deformed dark schists and sandstones of the Primary 3. Tizi n’Test route: first small massifs of primary rocks (Guemassa), then the red series and Primary rocks as on the Tizi n’Tichka route. Fossils and minerals Primary: trilobites (actually collected further south in the same land) Secondary: quartz geodes (amethyst) in the volcanic flows of the Triassic To know more… Piqué A. (1994) – Geology of Morocco. Pumag, Rabat. Saadi M. (1982) – Structural map of Morocco. Ministry of Energy and Mines, Rabat. Mount Toubkal featured treks:   Toubkal National Park summer Trek 8 days From the Atlas to the heart of the medina of Marrakech, this Moroccan adventure offers us an astonishing combination of sporting challenge, magical encounters and spectacular landscapes. We will experience the hospitality of the Berber people in the High Atlas region where the highest peaks are located, including Toubkal at 4,167 m … From the top, the reward is fantastic: a panorama over the whole region. Day 1:Marrakech – Imlil (1750m) – Camp of Toubkal (3200m) Transfer to Imlil, from where we will start our trek. We will first cross magnificent gardens and apple and walnut orchards to arrive in Aremd. Our path continues on a mule trail very popular with pilgrims from Sidi Chamharouch, marabout confined under a white rock at the corner of the two wadis. Continue to the two shelters to camp nearby. Dinner and overnight in tents. Walking time: 5h. Elevation: + 1450m. Transfer time: 1h30 Day2: Ascent of Toubkal (4167m) Departure at dawn by a steep and rocky path without any difficulty to arrive at the highest peak of Morocco and North Africa. Magnificent view on the chain of the High Atlas and the neighboring valleys, the Siroua and the borders of the desert. Descent to base camp. Dinner and overnight in tents. Walking time: 5 to 6 hours. Difference in height: + 1000m / – 1000m. Day3: Ascent of Timzguida Ouanoukrim (4089m) and Ras Ouanoukrim (4083m) Very early departure for the ascent of the second highest peak of the Atlas. Climb to the Tizi Ouaguane pass (3750m). Passage through

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