Ad
related to: diagram of a cirque del riotickets-center.com has been visited by 1M+ users in the past month
Search results
Results From The WOW.Com Content Network
Pyramidal peak. The Matterhorn, a classic example of a pyramidal peak. A pyramidal peak, sometimes called a glacial horn in extreme cases, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point. Pyramidal peaks are often examples of nunataks.
A model attribution edit summary is Content in this edit is translated from the existing Spanish Wikipedia article at [[:es:Línea 7 del Metro de la Ciudad de México]]; see its history for attribution. You may also add the template {{Translated|es|Línea 7 del Metro de la Ciudad de México}} to the talk page.
A cirque (French: [siʁk]; from the Latin word circus) is an amphitheatre -like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic: coire, meaning a pot or cauldron) [1] and cwm (Welsh for 'valley'; pronounced [kʊm]). A cirque may also be a similarly shaped landform arising from fluvial erosion.
Due to the subsidence of the city, there have been problems with the elevated portion of the line (which runs from Pantitlán to Velódromo stations). Following the collapse of a Mexico City Metro overpass in 2021, these concerns increased when commuters reported plainly visible deformations in the bridge connecting the Pantitlán and Puebla stations. [4]
Alegría (Cirque du Soleil) Alegría. (Cirque du Soleil) Alegría is a Cirque du Soleil touring production, created in 1994 by director Franco Dragone and director of creation Gilles Ste-Croix. It takes its name from the Spanish word for "joy". Since April 1994 the show has been performed over 5000 times, and has been seen by over 14 million ...
Glacial landform. Glacial landforms are landforms created by the action of glaciers. Most of today's glacial landforms were created by the movement of large ice sheets during the Quaternary glaciations. Some areas, like Fennoscandia and the southern Andes, have extensive occurrences of glacial landforms; other areas, such as the Sahara, display ...
At the start of a classic valley glacier is a bowl-shaped cirque, which have escarped walls on three sides but is open on the side that descends into the valley. Cirques are where ice begins to accumulate in a glacier. Two glacial cirques may form back to back and erode their backwalls until only a narrow ridge, called an arête is left.
Line B under construction over Avenida Central in Ciudad Nezahualcóyotl.. Line B was planned as a feeder line that would connect Mexico City to the adjacent municipalities of the State of Mexico, such as Ecatepec de Morelos and Ciudad Nezahualcóyotl, therefore, instead of using the same numbering system as with the other metro lines, the line was named as Line B, same as in Line A, which ...