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  2. Spanish Peaks Wilderness - Wikipedia

    en.wikipedia.org/wiki/Spanish_Peaks_Wilderness

    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.

  3. List of mountains in Spain - Wikipedia

    en.wikipedia.org/wiki/List_of_mountains_in_Spain

    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]

  4. Help:IPA/Spanish - Wikipedia

    en.wikipedia.org/wiki/Help:IPA/Spanish

    For a guide to adding IPA characters to Wikipedia articles, see Template:IPA, and Wikipedia:Manual of Style/Pronunciation § Entering IPA characters. For terms that are more relevant to regions that have not undergone yeísmo (where words such as haya and halla are pronounced differently), words spelled with ll can be transcribed in IPA with ʎ .

  5. Torres del Paine National Park - Wikipedia

    en.wikipedia.org/wiki/Torres_del_Paine_National_Park

    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.

  6. Geology of the Iberian Peninsula - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Iberian...

    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.

  7. Spanish Peaks - Wikipedia

    en.wikipedia.org/wiki/Spanish_Peaks

    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 ...

  8. Spanish phonology - Wikipedia

    en.wikipedia.org/wiki/Spanish_phonology

    The phone occurs as a deaffricated pronunciation of /tʃ/ in some other dialects (most notably, Northern Mexican Spanish, informal Chilean Spanish, and some Caribbean and Andalusian accents). [14] Otherwise, /ʃ/ is a marginal phoneme that occurs only in loanwords or certain dialects; many speakers have difficulty with this sound, tending to ...

  9. Montserrat (mountain) - Wikipedia

    en.wikipedia.org/wiki/Montserrat_(mountain)

    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]