A damaging earthquake of magnitude 6.4 mb (USGS) rocked the Garhwal region on 29 March, 1999 at 00:35:00 hours (IST). Maximum intensities of VIII and VII on the Medvedev–Sponheaer–Karnik (MSK-64) scale and the European Macroseismic Scale-98 (EMS-98) were observed in the affected region. Extensive damage was noticed both in the Chamoli and Rudraprayag regions of the Garhwal Himalaya. In the Chamoli region, damage of intensity VIII was confined to the right bank of the river Alaknanda. In the Rudraprayag region, the damage was widespread between Chandrapuri and Cantha villages. An isoseismal map prepared on the basis of a damage survey shows a NW–SE trend with its major axis in the NW–SE direction and minor axis in the NE–SW direction in the Rudraprayag region. The major axis is 11 km long and minor axis 8 km long. Thus the VIII isoseismal zone covers an area of approximately 88 km 2. The damage survey revealed that maximum damage has been either along major faults or to adobe houses, locally called Pathal houses. The damage was also higher than expected because of the use of undressed stones and heavy Pathal (slate) roofing. The villages of Kansali, Pingalpani, Akhori, Kiyunja, Sena, Cantha, Tewri, Talsari, and Chamoli were the most affected in the Rudraprayag and Chamoli regions. Grade 4 and Grade 3 damage has been observed in many adobe houses in the intensity zone VII. The study of damage distribution and intensity attenuation has demonstrated an asymmetric distribution and heterogeneous behaviour. The heterogeneous pattern could be related to rupture asperity distribution. A noteworthy feature of this earthquake was that it has produced a lot of ground fissures, some traceable for many tens to hundreds of meters affecting both rocks and overburden. One such fissure was traced for nearly 500 m trending NW–SE with a downthrow of 20–25 cm. This fissure shows thrust faulting with the foot wall having moved down towards the NE and the hanging wall upwards toward the SW side. This is in conformity with the fault plane solution given by the USGS using the moment tensor technique, which indicates that the earthquake originated by slip along a low angle thrust fault dipping NE. Changes in hydrological conditions have been noticed in a number of villages, for example Kiyunja, Kansali, Talsari, Pingalpani, Mukku, Sena, Akhori, Tewri, Gurpunga and Bhatwari etc.