GEOGRAPHIC SITUATION

    The municipality of Agolada is placed in the geographical center of Autonomous Community, in the Northeast of the province of Pontevedra, between the Ulla river, Farelo's mountain range, and the Arnego river.

Official route map

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   The municipality is 147,820 square Kilometers with a great morphological variety in its lands. This variety is due more to tecthonic factors that to the lithologic ones. The masterlines are configurated by three elements:
        - Farelo mountain range.
        - Soft ondulations of high surfaces of erosion.
        - Ulla river and its tributary, Arnego river.
   

 
   
The highest point is placed in Farelo mountain range which highest height is Farelo mountain with 956 meters. From here the heights descend softly across two erosion surfaces, one of them in direction E-W to the Arnego river and the another one in direction NW-SE to the right side of Ulla river, where the heigth is fixed in 300 meters. These differences of heigth explain the existence of local microclimates.

 

 

     The main units of relief are organized in a general direction NW-SE. These direction lines are crossed by the tributary rivers of Ulla river (Deza and Arnego).  
   The river system is organized around of two main courses, Ulla and Arnego. The Ulla river, that acts as the municipality north border, has a general direction E-W. Several rivers discharge their waters on it; between their, the main is the Arnego river, which, across the municipality make a straigth valley with strong slopes, in direction NW-SE to discharge in Ulla river in Brocos, that make the begining of Portodemouros reservoir.    
 

 

Cimate in Agolada, is oceanic type, modified by the indoor situation, that has relatively soft temperatures in winter, mainteining a standard temperature in the coldest month upper to 6 ºC, and fresh summers in that rarely the temperature is upper 17ºC as standard. Heigth and direction about normal atmospheric actions determinate this climatology.

    The annual rainfalls are fixed in 1.290 milimeters, with a pluviometric status based in winter maximum and summer minimum very strong.