(long term) <span>forecast are usually less accurate than (short term) forecast.</span>
Answer:
In topographical terms, the Massif Central is land lying mostly at above 500 metres, and includes most of the regions of Auvergne and Limousin, plus parts of the regions of Rhone-Alpes, Languedoc, and Midi-Pyrenees.
Occupying about one-sixth of France (33,000 square miles [86,000 square km]), the massif, for the most part, consists of plateaus lying between 2,000 and 3,000 feet (600 and 900 m).
In the altitudinal zonation of the equatorial mountain areas of Latin America, the zone between 3,000 to 6,500 feet (1,000 to 2,000 m) with warm temperate conditions and deciduous forest is the tierra templada.
What is the meaning of tierra templada?
a region or zone of temperate climate especially : tropical land of usually from 2000 to 6000 foot elevation in which the temperature is modified by the elevation.
What vegetation is in the tierra templada?
Tierra templada (temperate land) is the area between 900 and 1800 m (3000 to 6000 ft) where mean annual temperatures are usually between about 18°C and 25°C (64°F to 77°F). The natural vegetation in these zones is temperate forest, such as oak and pine-oak forest.
Learn more about tierra templada:
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<u>Answer:
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The ranking of common igneous silicate minerals based on the temperature at which crystallization occurs is called Bowen’s reaction series.
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Explanation:
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In Bowen’s reaction series the minerals with high crystallization temperature are present at the top layer. This means these minerals are the first to crystallize from the magma and they are mostly unstable. The Bowen's reaction series is represented in the Y shape. The left branch of this Y has minerals containing iron and magnesium. They are called as Ferromagnesium minerals.
The right branch of the Y contains plagioclase feldspars minerals. Temperature gradually decreases down along the Bowen’s reaction series from 
to 
. At certain low temperature, the two branches combine forming minerals similar to felsic rocks such as orthoclase feldspar, quartz and muscovite mica.
The places by the equator are hot because the sun's rays are by or directly on the equator.
