TOPOGRAPAHY
The topography of Antipolo may be described as generally hilly and mountainous, the hilly portions lying in the west and the mountainous area concentrated in the east as part of the Sierra Madre Mountain Range. Well-watered valleys are located in the middle of the city and in the northern and southern edges. Plateaus of over 200 meters above sea level are seen in the western half of the study area, including the site of the Poblacion and portions of Brgy. Cupang and San Juan. In the eastern half, these are seen in Brgys. Calawis and San Jose overlooking the Boso-Boso River Valley to the west.
CLIMATE
Based on PAGASA (Philippine Atmospheric, Geophysical and Astronomical Service Administration) Antipolo has Type I Climate which is marked by two (2) distinct seasons the Wet from May to December and the Dry from January to April. The main climatic control operating in the climate of the area is actually the monsoon wind system. The warm southwest monsoon wind brings the rain to the city after gathering moisture from the Indian Ocean while the cool northeast monsoon moves as a dry wind and comes even drier after crossing the Sierra Madre geographic barrier.
Source: City Planning and Development Office


