Weathering is the process through which the surface minerals of rock are broken down and loosened. This occurs through the action of extreme temperatures, rainwater and biological activity.
Thus, softer, porous or more permeable rocks are more susceptible to the mecahnical action of water and wind. This leads to them <em>weathering faster</em>.
Warmer climates generally have larger amounts of rainfall. This leads to rocks in these areas to <em>weather faster</em> than rocks in colder climates.
Rocks with slowly dissolving minerals are <em>more resistant</em> to weathering than other rocks due to increased resistance to the chemical effects of water.
The more water present, the <em>higher</em> the effect of chemical and physical withering.
More permeable rocks are <em>less resistant </em>to weathering due to the fact that more water can penetrate and thus erode the rock.
In conclusion, the explaining statements are numbers 1, 2 and 4. Statements 3 and 5 are <em>false.</em>