Temat: Central High-Atlas - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: A preliminary report on dinosaur track assemblages from the Middle Jurassic of the Imilchil area, Morocco
Autorzy:: Gierliński, G. D.
Menducki, P.
Janiszewska, K.
Wicik, I.
Boczarowski, A.
Powiązania:: https://bibliotekanauki.pl/articles/2059246.pdf
Data publikacji:: 2009
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: dinosaur tracks
Bathonian
Bajocian
Central High Atlas
Morocco
Opis:: Dinosaur tracks are reported from three new localities near Imilchil, in the Central High Atlas of Morocco. New dinosaur track assemblages are recognized in Bathonian and Bajocian beds. The Bathonian track assemblage comprises theropod, sauropod and ornithopod footprints. The Bajocian deposits contain a sauropod-thyreophoran track assemblage.
Źródło:: Geological Quarterly; 2009, 53, 4; 477-482
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: The karst landscapes of Beni Mellal Atlas (central Morocco): identification for promoting geoconservation and tourism
Autorzy:: Barka, Abdellah Ait
Rais, Jamila
Barakat, Ahmed
Louz, Elhassan
Nadem, Samir
Powiązania:: https://bibliotekanauki.pl/articles/15804900.pdf
Data publikacji:: 2022
Wydawca:: Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:: karst landscapes
geo-tourism
Central High Atlas
Atlas of Beni Mellal
Opis:: The Atlas of Beni Mellal is located in the Moroccan central High Atlas, characterized by an important geo-di-versity that attracts tourists every year. However, the number of visitors remains limited due to the lack of the promo-tion means, enhancement and mediation of this heritage. The obtained data indicate that the studied area preserves a great number of karst geosites, such as ruiniform landscapes, caves, poljes, sinkholes, Karren, shaft cave and many remarkable reliefs such as canyons and cliffs. This work concerns the inventory, the quantitative evaluation and the en-hancement of the remarkable geomorphosites. The results reveal the presence of 21 sites, including six karst forms; five ruiniform landscapes and one karren form, one enviable panoramic viewpoint and five karst springs, four caves, two travertines, two waterfalls, and one structural relief geosite; canyon, and one tepee structures. However, these sites are not protected against all types of degradation, because the general public does not recognize them. These karst forms are very vulnerable, they cannot reproduce quickly, and their deterioration leads to their permanent disappearance. That is why this heritage must be the object of a particular attention of the whole community. The valorisation of these geomorphologic assets is the proposal of a number of circuits and geotourist routes from the perspective of local and integrated development.
Źródło:: Quaestiones Geographicae; 2022, 41, 3; 87-109
0137-477X
2081-6383
Pojawia się w:: Quaestiones Geographicae
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: Integrated biostratigraphy across the Aalenian/Bajocian boundary of the Central High Atlas, Morocco
Autorzy:: Sadki, D.
Powiązania:: https://bibliotekanauki.pl/articles/2077320.pdf
Data publikacji:: 2015
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Aalenian/Bajocian boundary
Central High Atlas
Morocco
integrated biostratigraphy
Aalen
Bajos
Atlas Wysoki
Maroko
biostratygrafia
Opis:: This work presents an integrated biostratigraphic study across the Aalenian/Bajocian boundary of the Central High Atlas of Morocco. The data that are the basis for this study were obtained from the region of Rich that is located in the center of the basin of the Moroccan High Atlas. This region presents a thick Aalenian–Bajocian succession with continuous marine sedimentation, which offers a rich and varied fauna whose analysis enables the compilation of an integrated biostratigraphy based on the different paleontological groups: ammonites, belemnites, brachiopods, bivalves, gastropods, calcareous nannofossils, foraminifera and ostracods.
Źródło:: Volumina Jurassica; 2015, 13, 1; 27--42
1896-7876
1731-3708
Pojawia się w:: Volumina Jurassica
Dostawca treści:: Biblioteka Nauki

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