Climates that are warm and moist will produce more chemical weathering than do cool dry areas. Rocks in cold dry and hot dry areas/weather generally experience more mechanical weathering than chemical weathering.
That's a potentially complex answer. You need to look at the factors that control weathering - climate, slope, vegetation, overburden, bioturbation, rock mineralogy, rock structure, latitude, topography...
The reason it differs is because when it is at the top of a mountain, the air is much colder. The air penertrates the pours (holes) in the rocks and it causes it to slowly crack and eventually break completely.
At sea level it is not as cold, but when the water continuously hits the rocks, some of the particles in the rocks break away.
When a rock is warm, the Particles in it expand and when a rock is cold the particles in it contract. Because it is constantly expanding and contracting, it makes the rock weaker and eventually it will break.
Yes, it depends on the type of rocks, but in general rocks weather at a faster rate in areas were it is warmer and more moist.
Chemical weathering is the most effective in hot and dry climates. This is because this climate accelerates and intensifies the chemical weathering.
a moist dry climate
uplift-weathering hypothesis is a “proposal that chemical weathering is an active driver of climate change, rather than just a negative feedback that moderates climate". uplift-weathering hypothesis both discuss how chemical weathering is a negative feedback that moderates climate; however, the uplift hypothesis tries to say that chemical weathering is the active driver for climate change and not just a negative feedback
how fast weathering occurs depends on the CLIMATE of an area.
You can look it up in Uranus
Chemical weathering is most common in warm and wet climate.
in a warm humid climate it is mostly mechnical weathering but in a dry climate it is mostly chemical weathering.
The climate that is the most conducive to rapid weathering are tropical climates. They will have the fastest rate of weathering.
Chemical weathering is the most effective in hot and dry climates. This is because this climate accelerates and intensifies the chemical weathering.
rain
chemical weathering
weathering occurs faster in warm and rainy climate. the rate of which soil forms depends on the climate and type of rock. so soil formation is faster when weathering is quicker too.
a moist dry climate
uplift-weathering hypothesis is a “proposal that chemical weathering is an active driver of climate change, rather than just a negative feedback that moderates climate". uplift-weathering hypothesis both discuss how chemical weathering is a negative feedback that moderates climate; however, the uplift hypothesis tries to say that chemical weathering is the active driver for climate change and not just a negative feedback
how fast weathering occurs depends on the CLIMATE of an area.
Mechanical weathering refers to weathering that causes physical erosion of exposed rock without changing its chemical composition. Climate helps promote or prevent things like frost and wind that create this form of weathering.
Mechanical weathering refers to weathering that causes physical erosion of exposed rock without changing its chemical composition. Climate helps promote or prevent things like frost and wind that create this form of weathering.