Respuesta :
The rocks are still close to their original location. Iron in the rocks has weathered due to oxygen exposure. Weathering can result from a reaction between the minerals in the rock and precipitation. so, its true.
The internal structure of a rock influences how susceptible it is to weathering. While layered sedimentary rocks have bedding planes that are easily ripped apart and penetrated by water, massive rocks like granite typically do not have these weak points. The rate of weathering will be fastest in an area with a warm, humid climate.
A warmer environment will support a wider variety of vegetation, and biological weathering will occur more quickly. This occurs as a result of the rapid growth and multiplication of bacteria and plants in warmer environments. Chemical weathering is the term used to explain how chemicals in rainwater alter the minerals in a rock. Rainwater becomes slightly acidic as a result of the air's carbon dioxide being dissolved in it.
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Correct Question:
The rocks have not moved very far from their source the rocks contain iron that has weathered in the presence of oxygen. State true or false.
