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The Causes of Foehn Warming in the Lee of Mountains
The foehn effect is well known as the warming, drying, and cloud clearance experienced on the lee side of mountain ranges during “flow over” conditions. Foehn flows were first described more than a century ago when two mechanisms for this warming effect ...
A. Elvidge, I. Renfrew
semanticscholar +1 more source
Characteristic trajectories of ecosystem services in mountains
Intensification of land use and management over recent decades has resulted in trade-offs between food or timber production and other ecosystem services (ES). Despite an increase in scholarly publications on ES, the temporal aspects of ES trade-offs have
B. Locatelli+4 more
semanticscholar +1 more source
Известия Томского политехнического университета. Инжиниринг георесурсов. Т. 332, № 7 [PDF]
core +1 more source
Uplift-driven diversification in the Hengduan Mountains, a temperate biodiversity hotspot
Yaowu Xing, Richard H. Ree
semanticscholar +1 more source
Single-crystal FTIR and X-ray study of vishnevite, ideally [Na6(SO4)][Na2(H2O)2](Si6Al6O24)
This paper reports a single-crystal FTIR spectroscopic study of vishnevite, ideally [Na6(SO4)] [Na2(H2O)2](Si6Al6O24), a member of the cancrinite group of feldspathoids.
BELLATRECCIA, FABIO+4 more
core
Narrow thermal tolerance and low dispersal drive higher speciation in tropical mountains
N. Polato+17 more
semanticscholar +1 more source
The Rwenzori Mountains, a landslide-prone region?
L. Jacobs+5 more
semanticscholar +1 more source
Kobyashevite, Cu5(SO4)2(OH)6·4H2O, a new devilline-group mineral from the Vishnevye Mountains, South Urals, Russia [PDF]
A new mineral kobyashevite, Cu5(SO4)2(OH)6·4H2O (IMA 2011–066), was found at the Kapital’naya mine, Vishnevye Mountains, South Urals, Russia. It is a supergene mineral that occurs in cavities of a calcite-quartz vein with pyrite and chalcopyrite. Kobyashevite forms elongated crystals up to 0.2 mm typically curved or split and combined into thin crusts ...
Dmitry Yu. Pushcharovsky+7 more
semanticscholar +5 more sources
Mineral zoning in fenites around miaskite intrusions of the Vishnevye Mountains complex can be interpreted as a magmatic-replacement zonal metasomatic aureole (in D.S. Korzhinskii’s understanding): the metasomatic transformations of the fenitized gneisses under the effect of deep alkaline fluid eventually resulted in the derivation of nepheline syenite
S. S. Abramov+2 more
semanticscholar +4 more sources