Search results
Results from the WOW.Com Content Network
The Spanish Peaks are geologically distinct from the faulted and uplifted mountains of the Sangre de Cristo range to the west. To the geologist the Spanish Peaks are prime examples of "stocks" which are defined as large masses of igneous (molten) rock which intruded layers of sedimentary rock and were later exposed by erosion.
Pico de Peñalara, 2428 m, the highest of Sierra de Guadarrama La Sagra, at 2383 m is the highest mountain of the Prebaetic System. Puig Major, 1445 m, the highest of Balearic Islands. This is a list of Spanish mountains with their elevation taken from the Instituto Nacional de Estadística de España data. [1]
The Douro Basin in northwest Spain is the largest Cenozoic basin in Iberia. Oligocene and Miocene continental deposits are up to 2.5 km thick. It is bounded by the central system to the south, the Iberian range to the east, and the Cantabrian Mountains to the northeast. The Cantabrian Mountains are the main source of the sediments in this basin.
Torres del Paine National Park (Spanish: Parque Nacional Torres del Paine) [3] is a national park encompassing mountains, glaciers, lakes, and rivers in southern Chilean Patagonia. The Cordillera del Paine is the centerpiece of the park. It lies in a transition area between the Magellanic subpolar forests and the Patagonian Steppes.
The mountain is composed of strikingly pink conglomerate, a form of sedimentary rock. Montserrat was designated as a National Park in 1987. The Monastery of Montserrat which houses the virgin that gives its name to the monastery is also on the mountain, although it is also known as La Moreneta ("the little tan/dark one" in Catalan). [2]
The Spanish Peaks are situated 100 miles (160 km) due south of Colorado Springs. The Spanish Peaks were formed by two separate shallow (or hypabyssal) igneous intrusions during the Late-Oligocene epoch of the Paleogene Period. [2] [3] West Spanish Peak is an older (24.59 +/- 0.13 Ma) quartz syenite. East Spanish Peak (23.36 +/- 0.18 Ma) is ...
In general usage, a cuesta is a hill or ridge with a gentle slope (backslope) on one side, and a steep slope (frontslope) on the other. The word is from Spanish: "flank or slope of a hill; hill, mount, sloping ground". In geology and geomorphology, cuesta refers specifically to an asymmetric ridge with a long and gentle backslope called a dip ...
In standard European Spanish, as well as in many dialects in the Americas (e.g. standard Argentine or Rioplatense, inland Colombian, and Mexican), word-final /n/ is, by default (i.e. when followed by a pause or by an initial vowel in the following word), alveolar, like English [n] in pen. When followed by a consonant, it assimilates to that ...