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NEG se CL puede can. 1SG pisar walk el the césped grass No se puede pisar el césped NEG CL can.1SG walk the grass "You cannot walk on the grass." Zagona also notes that, generally, oblique phrases do not allow for a double clitic, yet some verbs of motion are formed with double clitics: María María se CL fue went.away- 3SG María se fue María CL went.away-3SG "Maria went away ...
The Diccionario esencial de la lengua española (Essential Dictionary of the Spanish Language) was published in 2006 as a compendium of the 22nd edition of the Dictionary of the Spanish Language. [19] Ortografía de la lengua española (Spanish Language Orthography). The 1st edition was published in 1741 and the latest edition in 2010.
Ortografía de la lengua española (2010). Spanish orthography is the orthography used in the Spanish language.The alphabet uses the Latin script.The spelling is fairly phonemic, especially in comparison to more opaque orthographies like English, having a relatively consistent mapping of graphemes to phonemes; in other words, the pronunciation of a given Spanish-language word can largely be ...
Although the term altitude is commonly used to mean the height above sea level of a location, in geography the term elevation is often preferred for this usage. In aviation, altitude is typically measured relative to mean sea level or above ground level to ensure safe navigation and flight operations.
The term elevation is mainly used when referring to points on the Earth's surface, while altitude or geopotential height is used for points above the surface, such as an aircraft in flight or a spacecraft in orbit, and depth is used for points below the surface. Elevation histogram of the Earth's surface
Don't worry about relying on your browser's spell check feature. With AOL Mail, click one button to check the entire contents of your email to ensure that everything is spelled correctly. In addition, you'll never need worry about typos or misspelled words again by enabling auto spell check. Use spell check
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 ...
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