they can leak discharge
Climate, soil, temperature, water, clouds, rocks, etc.
tere mare many rocks but alll rocks are like rocks they always bscome rocks and roks say with me rocks remains rocks rocks remains rocks rocks remains rocks rocks remains rocksrocks remains rocks rocks remains rocks rocks remains rocks rocks remains rocks rocks remains rocksrocks remains rocksrocks remains rocks vrocks remains rocks v rocks remains rocksrocks remains rocksrocks remains rocksrocks remains rocks v rocks remains rocksrocks remains rocks rocks remains rocksrocks remains rocksrocks remains rocks rocks remains rocksrocks remains rocksrocks remains rocksrocks remains rocksrocks remains rocksvrocks remains rocksrocks remains rocksrocks remains rocks v vrocks remains rocksrocks remains rocks rocks remains rocksrocks remains rocksrocks remains rocksvrocks remains rocks rocks remains rocks rocks remains rocksrocks remains rocks v v rocks remains rocks rocks remains rocks v rocks remains rocks rocks remains rocksrocks remains rocksrocks remains rocksrocks remains rocksrocks remains rocksrocks remains rocksrocks remains rocksrocks remains rocksrocks remains rocks
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rocks and minerals
No. Volcanic rocks are made of the same materials that other rocks are.
There are two effects of carbonate rocks to the global climate. The two effects of carbonate rocks to the global climate are dissolution and deposition.
when it is in a humid climate
Dry Climates
The rate at which rocks weather is determined by factors such as the type of rock, climate (temperature and precipitation), presence of vegetation, and human activities. Rocks that are more susceptible to chemical and physical breakdown will weather faster compared to more resistant rocks.
rocks an fossils
water, fog ,rocks,climate,
a metamorphic rock which has been changed by climate ,pressure or acid in things like rain.Example of metamorphic rocks;Slate and Marble. Hope I helped answer your question.
Different types of rock layers, such as sedimentary rocks like limestone or sandstone, can provide information about past climates based on the fossils they contain. For example, the presence of tropical plant fossils in certain layers indicates a warm climate. Additionally, the ratio of certain isotopes in rocks can also provide clues about past temperatures and climate conditions.
Chemical weathering is generally more active in a temperate climate due to higher levels of moisture and precipitation, which can break down rocks through processes like hydration and oxidation. In contrast, desert climates often have lower precipitation levels, resulting in slower rates of chemical weathering on rocks.
Sedimentary rocks are likely to form in a lake in a hot climate. The heat can lead to evaporation of water, leaving behind sediments that can accumulate and eventually become compacted and cemented into sedimentary rocks.
At sea shores in a humid climate growing on large flat rocks.
Climate, soil, temperature, water, clouds, rocks, etc.