A cavity type tube well draws water from the bottom of the well where a hollow cavity has formed, rather than from the sides of the well like a standard tube well. The cavity forms as fine sand is pumped out with the initial water, leaving an empty space. This cavity increases the area available to draw water from, allowing more water to enter the well through a reduced velocity. Cavity wells are drilled into permeable unconfined aquifers and do not require a strainer, drawing water from a single stratum where the cavity has formed.