Macizo wikipedia

This file contains additional information, probably added from the digital camera macizo wikipedia scanner used to create or digitize it. If the file has been modified from its original state, some details may not fully reflect the modified file. This is a file from the Wikimedia Commons and may be used by other projects, macizo wikipedia. Information from its description page there is shown below.

Macizo de Anaga is a mountain range in the northeastern part of the island of Tenerife in the Canary Islands. The highest point is 1, m Cruz de Taborno. It stretches from the Punta de Anaga in the northeast to Cruz del Carmen in the southwest. The mountains were formed by a volcanic eruption about 7 to 9 million years ago making it the oldest part of the island. It is a remote and wild area characterized by humid forests, such as laurisilva. Native plant species include Ceropegia dichotoma , Ceropegia fusca and Echium virescens. A place in the mountains known as El Bailadero is believed to have been a place where witches were practicing witchcraft and dancing around a bonfire.

Macizo wikipedia

Macizo de la Maladeta is the highest mountain range and the first glacial massif in the Pyrenees. It is located in the Spanish province of Huesca Aragon. To the north is the head of the Benasque Valley , and to the south the Vallibierna Valley descends. The name Maladeta was known at the start of the 18th century [1] and the legend of the curse was already very strong. The latest studies published in and indicate an Aragonese word, uncertainly related to the Latin maledicta "cursed" but the association of the preindo-European and precelte root Mal "high rocky mountain" at the root dicta advanced by P. Dauzat remains doubtful. This article about a location in Aragon, Spain, is a stub. You can help Wikipedia by expanding it. Contents move to sidebar hide. Article Talk. Read Edit View history. Tools Tools. Download as PDF Printable version. In other projects. Wikimedia Commons.

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Its highest point is Pena Trevinca at 2, metres 6, ft. Another important peak is Cabeza de Manzaneda 1, m. Its eastern end merges with the Cantabrian Mountains. The relief of the system, with an average height of metres 1, ft , is relatively smooth compared with other Iberian ranges. It is however very complex, having no defined structural alignment owing to the heavy fluvial erosion that has fragmented the terrain. Generally the system includes mountains that are rounded in shape, often topped by small rocky outcrops, as well as horsts , basins and faults , roughly aligned in a N-S direction. Since rain is abundant in Galicia, the undisturbed areas of the massif have a soft soil texture and are covered in dense vegetation of temperate deciduous forest where Quercus petraea and Quercus robur oaks predominate.

Macizo de Anaga is a mountain range in the northeastern part of the island of Tenerife in the Canary Islands. The highest point is 1, m Cruz de Taborno. It stretches from the Punta de Anaga in the northeast to Cruz del Carmen in the southwest. The mountains were formed by a volcanic eruption about 7 to 9 million years ago making it the oldest part of the island. It is a remote and wild area characterized by humid forests, such as laurisilva. Native plant species include Ceropegia dichotoma , Ceropegia fusca and Echium virescens. A place in the mountains known as El Bailadero is believed to have been a place where witches were practicing witchcraft and dancing around a bonfire. Contents move to sidebar hide. Article Talk. Read Edit View history.

Macizo wikipedia

It is a dome-shaped region approximately 10 miles 16 km across and rising about 14, feet 4, m from the sea floor. The highest point of the massif is around metres 2, ft beneath the surface. It is believed that the massif was formed underneath the nearby Mid-Atlantic Ridge but was pulled from under the ridge during the movement of the plates , about 1. Geologic studies of the massif have indicated that it is not composed of the black basalt typical of the ocean floor but rather of dense green peridotite , which is usually found in the mantle. The central dome is corrugated and striated in a way that is representative of an exposed ultramafic oceanic core complex. An expedition to the area in made an important advance in the study of the ocean floor. It found that a steeply sloping detachment fault is associated with the oceanic core complex structure. The dome was caused by mantle material being extruded to the surface. Another expedition discovered the Lost City hydrothermal field near the summit of the ridge in

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Please help improve this article by adding citations to reliable sources. The following other wikis use this file: Usage on an. The Face on Mars is an example of an extraterrestrial massif. List of mountains in Aragon. It is however very complex, having no defined structural alignment owing to the heavy fluvial erosion that has fragmented the terrain. Generally the system includes mountains that are rounded in shape, often topped by small rocky outcrops, as well as horsts , basins and faults , roughly aligned in a N-S direction. This is a file from the Wikimedia Commons and may be used by other projects. Commons is a freely licensed media file repository. Creative Commons Attribution-ShareAlike 3. Wikimedia Commons. The volcanic massif, emerged during the last 5 to 7 million years, is furrowed by deep ravines and ends abruptly in the sea, in an area known as Los Gigantes, a series of high cliffs that plummet over the sea. Categories : Landforms Mountains. Topographic map of Galicia. Download as PDF Printable version.

Tamu Massif is a seamount in the northwest Pacific Ocean , [3] sitting atop a triple junction of mid-ocean ridges. The massif covers an area of about , square kilometres , sq mi.

Download as PDF Printable version. The relief of the system, with an average height of metres 1, ft , is relatively smooth compared with other Iberian ranges. Information from its description page there is shown below. This article is about a geological formation. Wikimedia Commons. Toggle limited content width. The following other wikis use this file: Usage on an. Toggle limited content width. Download as PDF Printable version. In the movement of the crust , a massif tends to retain its internal structure while being displaced as a whole. Wikimedia Commons. Do not translate text that appears unreliable or low-quality. Variscan orogeny. Please help improve this article by adding citations to reliable sources.