FREE BOOKS

Author's List




PREV.   NEXT  
|<   10   11   12   13   14   15   16   17   18   19   20   21   22   23   24   25   26   27   28   29   30   31   32   33   34  
35   36   37   38   39   40   41   42   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   >>   >|  
vely low connection with the Cordillera Volcanica, the Sierra de Coalcoman is isolated from other mountain ranges in southwestern Mexico. CLIMATE The climates in Michoacan vary from tropical in the lowlands to cool temperate at high elevations in the Sierra de Coalcoman and Cordillera Volcanica. The highest temperatures are known in the Balsas-Tepalcatepec Basin, where at Churumuco the mean annual temperature is 29.3 deg. C. and the range of monthly means is 3.5 deg. C. (Contreras, 1942). Frosts occur sporadically on the Mexican Plateau, and in the winter snow falls on the highest mountains. Precipitation varies geographically and seasonally. Most of the rain falls between June and October. In the Balsas-Tepalcatepec Basin rainfall in the rest of the year is negligible. The annual average rainfall at Coahuayana on the Pacific Coastal Plain is 871 mm. (Guzman-Rivas, 1957:52). In the Balsas-Tepalcatepec Basin rainfall seldom exceeds 800 mm. per year. In the mountains precipitation is heavier and somewhat more evenly distributed throughout the year, but still definitely cyclic. For example, Uruapan (elevation, 1500 meters) receives an average annual rainfall of 1674 mm. (Contreras, 1942). The prevailing winds are from the Pacific Ocean. The southern (windward) slopes of the Sierra de Coalcoman probably receive more rain than any other part of the state. The Balsas-Tepalcatepec Basin lies in a rain shadow of the Sierra de Coalcoman, and the Mexican Plateau lies in a somewhat less drastic rain shadow of the Cordillera Volcanica; these are the driest regions in the state. VEGETATION AND ANIMAL HABITATS For the purposes of this report I have adopted the classification of types of vegetation that seem to me most significant in terms of ecological distribution of reptiles and amphibians in Michoacan. These types are as follows: TEMPERATE (1000-4000 meters) Fir Forest (2400-4000 meters) Pine-oak Forest (1000-4000 meters) Mesquite-grassland (1500-2100 meters) TROPICAL (0-1000 meters) Arid Tropical Scrub Forest (0-1000 meters) Tropical Semi-deciduous Forest (150-600 meters) The vegetation of the Pacific Coastal Plain and the Balsas-Tepalcatepec Basin consists of arid tropical scrub forest, composed of deciduous trees, which in many places are stunted and widely spaced. In the dry season there is little cover provided by this forest. In the rainy season there is a sparse
PREV.   NEXT  
|<   10   11   12   13   14   15   16   17   18   19   20   21   22   23   24   25   26   27   28   29   30   31   32   33   34  
35   36   37   38   39   40   41   42   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   >>   >|  



Top keywords:

meters

 

Tepalcatepec

 

Balsas

 

Forest

 

Sierra

 

rainfall

 

Coalcoman

 

Pacific

 

annual

 
Volcanica

Cordillera
 
Contreras
 

Plateau

 
mountains
 

Tropical

 
shadow
 
Coastal
 

vegetation

 

average

 

Mexican


highest

 

tropical

 
season
 
forest
 

Michoacan

 

deciduous

 

report

 

adopted

 

widely

 

spaced


classification

 

purposes

 

ANIMAL

 

provided

 

drastic

 

sparse

 

driest

 
regions
 

VEGETATION

 

HABITATS


composed

 

TROPICAL

 
grassland
 

consists

 

Mesquite

 

TEMPERATE

 
reptiles
 
distribution
 

ecological

 
significant