One of the most important inheritances of climate quaternary is glacier geomorphology evidence in Iran. Identifying and demarcation of glacial landforms in highlands are the best evidences to recognize morph climatic and morph dynamic territories. The study aimed to determine the morphoclimatic and morphodynamic zones in the last glacier period and current boundaries in the Jajroud basin, and compare results with previous theories. Hence, by using satellite imageries, topographic maps, GIS geology software and field observations, the locations of cirques were identified and then by using Peltier method morphoclimatic and morphodynamic boundaries in quaternary, were determined. Method and data used in this study were mainly obtained from topographic maps, geology, satellite images, climate data temperature and monthly precipitation. Results show that low level of glacier areas already existed at height of 5220 meter, and levels of solifluction, pluvial and pediment are at 4000 meter height, fluvial at, 3400 meter, and pediment at 1565 meter respectively. Also in the last glacier period, the lowest level of glacial was respectively at 3900 meter, Solifluction at 3000 meter, and fluvial at 2000 meter. The results show that morpho dynamic and morphoclimatic levels were higher than former results attained by "Alborz Mountain researches".