The environmental impacts of rock blasting at the Babawa main quarry site in Gezawa, Kano State, Nigeria, were systematically assessed. Electrical resistivity tomography, spontaneous potential, and induced polarization methods were employed using a Wenner array configuration with electrode spacings of 5 m and 10 m. Data processing and inversion were conducted using RES2DINV, while spatial visualization was performed with Surfer v12. Subsurface characterization revealed three layers: a highly weathered basement (comprising clay and gravel materials), a partially weathered and fractured basement, and a fresh granitic basement. Low resistivity values ranging from 16 $\Omega \cdot \mathrm{m}$ to 200 $\Omega \cdot \mathrm{m}$ were observed from near-surface depths to approximately 25 m, indicating zones of intense weathering. In contrast, resistivity values exceeding 1000 $\Omega \cdot \mathrm{m}$ were interpreted as relatively intact granitic formations minimally affected by blasting activities. In terms of chargeability responses, low values corresponded to weak, fractured zones and higher values indicated more competent lithologies. Zones of elevated spontaneous potential anomalies were associated with potential fluid migration pathways, while low spontaneous potential values corresponded to relatively intact and impermeable regions. A consistent spatial correlation among electrical resistivity tomography, induced polarization, and spontaneous potential datasets was identified, confirming the presence of fractured zones radiating outward from the quarry site. Although these fractures were not found to extend to significant depths, repeated blasting activities appear to have exacerbated pre-existing structural discontinuities. Such conditions may pose risks to nearby infrastructure and groundwater systems if left unmonitored. It is therefore recommended that continuous geophysical monitoring and stricter regulation of blasting operations be implemented to mitigate long-term environmental and geotechnical hazards.