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Abstract
El Cerro de Huenes constituye una estribación montañosa importante de la vertiente Noroccidental de Sierra Nevada. Como macizo presenta una notable complejidad geomorfológica, lo que unido a la diferencia altitudinal entre las zonas basales y la cumbre, configura un territorio de una gran variedad florística y paisajística. Dos pisos bioclimáticos pueden diferenciarse en él, mesomediterráneo y supramediterráneo, en ambos predominan materiales geológicos de tipo básico, siendo muy limitados los de tipo ácido. La vegetación presente en el piso mesomediterráneo queda incluida en la serie bética basófilade la encina: Paeonio coriaceae-Querceto rotundifoliae S. La del piso supramediterráneo se incluye en la serie: Berberido hispanicae-Querceto rotundifoliae S. En la actualidad son escasos los restos de las formaciones naturales, ocupando amplias extensiones del territorio las repoblaciones forestales de Pinus sylvestris.
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