Convection currents in Pakistan occur primarily in the atmosphere and the Earth's crust. In the atmosphere, these currents are driven by temperature differences, leading to weather patterns such as monsoons and thunderstorms, particularly during the summer months. In geological terms, convection currents in the mantle contribute to tectonic activity, influencing seismic events and the formation of mountain ranges, including the Himalayas. Overall, these currents play a crucial role in both meteorological and geological processes in the region.
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