When water percolates down through the soil
True
An aquifer forms when groundwater pools between a permeable layer and an impermeable layer.
caves
Groundwater.
Limestone is the type of rock that is chemically weathered by acidic groundwater, leading to distinctive features such as karst landscapes, sinkholes, and caves. The acidic groundwater, often containing carbonic acid formed from carbon dioxide in the soil, dissolves the calcium carbonate in limestone, resulting in the erosion and creation of these geological formations. Over time, this process can lead to significant alterations in the landscape.
Forming in groundwater is a top hole idea
Geysers are, in fact, formed when groundwater is heated by nearby magma. They can also be formed by volcanic eruptions and earthquakes occasionally as well.
sinkhole
caves
A cave?
caves
True
An aquifer forms when groundwater pools between a permeable layer and an impermeable layer.
An aquifer forms when groundwater pools between a permeable layer and an impermeable layer.
it will subside and damage roads, bridges, buildings etc.
Groundwater is formed when precipitation seeps into the ground through soil and rocks, filling up the spaces between particles and forming underground reservoirs. This groundwater can be accessed through wells and springs for drinking water and other uses.
Caves and sinkholes are formed by the erosion of soft rock formations by flowing groundwater. Over time, the water dissolves and carries away the rock, creating these underground or surface features.