We use NH 3 inversion transitions to trace the dense gas in the NGC 1333 region of the Perseus molecular cloud. NH 3 (1,1) and NH 3 (2,2) maps covering an area of 102 square arcminutes at an angular resolution of ∼3.7 are produced by combining VLA interferometric observations with GBT single dish maps. The combined maps have a spectral resolution of 0.14 km/s and a sensitivity of 4 mJy/beam. We produce integrated intensity maps, peak intensity maps and dispersion maps of NH 3 (1,1) and NH 3 (2,2) and a line-of-sight velocity map of NH 3 (1,1). These are used to derive the optical depth for the NH 3 (1,1) main component, the excitation temperature of NH 3 (1,1), and the rotational temperature, kinetic temperature and column density of NH 3 over the mapped area. We compare these observations with the CARMA J=1-0 observations of N 2 H + and H 13 CO + and conclude that they all trace the same material in these dense star forming regions. From the NH 3 (1,1) velocity map, we find that a velocity gradient ridge extends in an arc across the entire southern part of NGC 1333. We propose that a large scale turbulent cell is colliding with the cloud, which could result in the formation of a layer of compressed gas. This region along the velocity gradient ridge is dotted with Class 0/I YSOs, which could have formed from local overdensities in the compressed gas leading to gravitational instabilities. The NH 3 (1,1) velocity dispersion map also has relatively high values along this region, thereby substantiating the shock layer argument.