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  • Understanding Aquifers: The Layers That Hold Groundwater
    The layers of porous material through which groundwater moves are called aquifers.

    Here's a breakdown:

    * Aquifer: A geological formation that can store and transmit groundwater. Aquifers are typically made up of porous and permeable rock, sediment, or soil.

    * Porosity: The amount of empty space within a material. Porous materials like sand and gravel have lots of space for water to fill.

    * Permeability: The ability of a material to allow fluids to flow through it. A material can be porous but not permeable (like clay), meaning it has empty spaces but doesn't let water pass through easily.

    Types of Aquifers:

    * Unconfined aquifer: An aquifer where the top of the water table is exposed to the atmosphere. Water can easily recharge these aquifers.

    * Confined aquifer: An aquifer that is sandwiched between two layers of impermeable rock or clay (like a sandwich!). The water pressure in a confined aquifer is higher than the surrounding atmosphere.

    Groundwater Movement:

    Groundwater flows through aquifers due to gravity and pressure differences. Think of it like a giant, slow-moving river underground.

    Let me know if you have any more questions about aquifers or groundwater!

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