By increasing the pressure on ice, its melting point

By increasing the pressure on ice, its melting point will; option [B] increase. Pressure influences the equilibrium between solid and liquid phases. When pressure rises, the equilibrium shifts towards the more densely packed solid phase. To maintain equilibrium, a higher temperature is required for the solid to melt into liquid, resulting in an increased melting point. This phenomenon is described by the Clausius-Clapeyron equation, which states that the melting point of a substance increases with increasing pressure. This relationship holds true for most substances, including ice. Therefore, as pressure on ice increases, its melting point increases accordingly. This principle has significant implications, especially in geology and glaciology, where understanding the effect of pressure on melting points helps explain phenomena like the behavior of glaciers under varying pressure conditions. It also has practical applications in industries such as food preservation and materials science, where precise control over melting points is necessary for manufacturing processes and product quality.