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The adjective is derived from Latinmontānus(“of or pertaining to a mountain”) + English-ane (variant of -an(suffix meaning ‘of or pertaining to’ forming adjectives)).[1]Montānus is derived from mōns(“mount, mountain”) (from Proto-Indo-European*men-(“to stand out, to tower”)) + -ānus(suffix meaning ‘of or pertaining to’).
This plant evidently occupies, like V. sabulosa and V. Curtisii, an intermediate position between lutea and tricolor; and, as I have indicated already, it is a montane, not an agrestal plant. Jordan compares it to V. vivariensis, which is also a montane plant, between V. tricolor and V. lutea.
[T]he upper part of these peaks is very bare and monotonous, and almost destitute of damp precipice; and I know of only seven Montane species that grow there above 650 yards.
With a like lower limit of level there are found on hills numerous Sub-alpine or Montane plants, which do not grow in the North. We must therefore divide the Northern zone also into three parts—1, Northern (restricted); 2, Northern-montane; and 3, Montane only.
The montane region in its lower belts has, at the equator, a still tropical although not equatorial character, but near the two tropics it has from the first a temperate character. The difference between the equatorial rain-forest of the basal region on the one hand, and the tropical forest of the lower montane region on the other, is confined to the systematic composition. In temperate montane formations, on the contrary, the lower temperature is reflected in purely oecological characteristics in the plant-life and impresses upon the formations the stamp of those of higher latitudes.
1914, Forrest Shreve, “The Physical Features of the Rain-forest Region”, in A Montane Rain-forest: A Contribution to the Physiological Plant Geography of Jamaica (Carnegie Institution of Washington Publication; no. 199), Washington, D.C.: Carnegie Institution of Washington, →OCLC, page 8:
The temperatures are extremely constant and low as compared with those in the lowlands, although very rarely so low as to make frost possible, and the rainfall is abundant at all seasons. The Blue Mountain Region is, therefore, a tropical montane region, in the terms of [Andreas Franz Wilhelm] Schimper, lying above the hot lowlands and not attaining to a sufficient altitude for alpine influences to come into full play.
1983, Jaclyn H. Wolfheim, “Indriidae: Avahi, Indris, and Sifakas”, in Primates of the World: Distribution, Abundance, and Conservation, Seattle, Wash.: University of Washington Press, →ISBN, page 121:
I[ndri] indri is a forest species, found in humid montane rain forest [...]. It has been observed as high as 1,300 m elevation [...].
The gorilla's ancestor had probably taken to the montane forests of a string of central African volcanoes, cutting itself off from the genes of other apes.
2000, M. Kappelle, M. E. Juárez, “Case Study: Mountain Forests, Biodiversity and People in Costa Rica”, in M. F. Price, N. Butt, editors, Forests in Sustainable Mountain Development: A State of Knowledge Report for 2000 (IUFRO Research Series; 5), Wallingford, Oxfordshire, New York, N.Y.: CABI Publishing, →ISBN, page 46:
The key to sustainable tropical montane cloud forest land management lies in actively involving local rural populations in decision-taking processes relating to research, training, development and conservation strategies and initiatives.
2014, Stephanie B. Jeffries, Thomas R. Wentworth, “Natural Community Overviews”, in Exploring Southern Appalachian Forests: An Ecological Guide to 30 Great Hikes in the Carolinas, Georgia, Tennessee, and Virginia (A Southern Gateways Guide), Chapel Hill, N.C.: University of North Carolina Press, →ISBN, page 22:
At lower elevations, montane oak forests typically grade into cove forests, oak forests, or montane pine forests and woodlands. At higher elevations and in more protected sites, northern hardwood forests replace the montane oak forests. Montane oak forests may also grade directly into spruce-fir forests on south-facing slopes.
1888, Frederic Arnold Lees, “Climatology”, in The Flora of West Yorkshire: With a Sketch of the Climatology and Lithology in Connection therewith (Botanical Series of the Transactions of the Yorkshire Naturalists’ Union; II), London: Lovell Reeve & Co.,, →OCLC, page 53:
The true Montanes comprise those species, of unmistakably Alpine, Scottish, or Highland type, which not merely with us but elsewhere throughout Britain are characteristic of high latitudes and altitudes—of mountain regions only.
2005, Peter Taylor, “Restoring Ecological Processes: Regeneration of the Core Vegetation”, in Beyond Conservation: A Wildland Strategy, London, Sterling, Va.: Earthscan, →ISBN, page 84:
The wintergreens, and northern montanes such as Linnaea have their stronghold in these pinewoods and some of their rarity may be due to the reduction in the extent of the forest.