Weathering and mass wasting on the Moon are minimal compared to Earth due to the lack of atmosphere and liquid water. The primary form of weathering on the Moon is mechanical, caused by micrometeorite impacts and thermal cycling, which can break down rocks over time. Mass wasting events, like landslides, are rare but can occur in the form of regolith movement due to impacts or seismic activity. Overall, the Moon's surface remains relatively stable compared to Earth’s dynamic environment.
No. The moon does not have a molten core for the plates to "float" on.
Not like on Earth. The moon has no atmosphere, so there is no wind or air at all to cause erosion. However, the moon is bombarded with objects in space that normally would burn up in our atmosphere, resulting in all of the craters that can be seen from the Earth.
What would you expect to find composite volcanoes on Mars? Explain why.
You would expect to find them in both.
Spring tides.
Chemical weathering is prevalent in tropical climates.
Panama
weathering could occur and the rock would break apart.
Certainly not haiti!
Chemical weathering of limestone would occur most rapidly in a warm and wet climate, where there is abundant rainfall and high temperatures to facilitate the dissolution and erosion of the limestone.
It will vary from leaching, weathering, and accumulation of organic matter.
Metabolism does not occur in the heart.
teeth
Many times it would rain but some times it would be very hot or partially warm
the rate of chemical weathering would slow down
Chemical weathering would occur rapidly in regions with high temperatures, abundant moisture, and acidic conditions. This includes tropical and subtropical regions with frequent rainfall, as well as areas with high levels of pollutants that contribute to the acceleration of chemical reactions on rocks and minerals.
Physical weathering is most likely to occur in climates with frequent temperature changes, such as in deserts and mountainous regions. These areas experience daily temperature fluctuations that contribute to the expansion and contraction of rocks, leading to physical weathering processes like freeze-thaw cycles and exfoliation.