In Dhunaghat area of Kumaun Lesser Himalaya, Precambrian greenschist m
etapelites of the Almora Group show evidence of contact metamorphism c
aused by intrusion of the hot Cambrian Champawat Granitoids plutonic b
ody. Mineral assemblages indicate hornblende-hornfels facies condition
s of contact metamorphism. Temperatures between 600 and 650-degrees-C
and pressures around 3 kb are suggested for the contact metamorphism.