Examine the diagram and the text:
The Water Cycle showing labels RECHARGE AREA, DISCHARGE AREA, PUMPED WELL, Water table, Days, Years, Unconfined aquifer, Confined aquifer, Confining bed, Centuries, and Millennia

The Water Cycle: Groundwater Discharge

There's more water than just what you can see

You see water all around you every day as lakes, rivers, ice, rain and snow. There are also vast amounts of water that are unseen—water existing in the ground. And even though groundwater is unseen, it is moving below your feet right now. As part of the water cycle, groundwater is a major contributor to flow in many streams and rivers and has a strong influence on river and wetland habitats for plants and animals. People have been using groundwater for thousands of years and continue to use it today, largely for drinking water and irrigation. Life on Earth depends on groundwater just as it does on surface water.

There are rivers flowing below our feet ... a myth?

Have you ever heard that there are rivers of water flowing underground? Do you think it is true? Actually, it is pretty much a myth. Even though there are some caverns, lava and ice tubes, and horizontal springs that can carry water, the vast majority of undergroundwater occupies the spaces between rocks and subsurface material. Some rivers, such as the Alapaha River in northern Florida, USA, can disappear underground during low-flow periods. Generally, water underground is more like water in a sponge. It occupies the spaces between soil and rock particles. At a certain depth below the land surface, the spaces between the soil and rock particles can be totally filled with water, resulting in an aquifer from which groundwater can be pumped and used by people.

Courtesy of the U. S. Geological Survey

Is there missing or extraneous information in this diagram? Are all of the details in the text relevant and accurate? Explain using details from the text.

The Water Cycle showing labels RECHARGE AREA, DISCHARGE AREA, PUMPED WELL, Water table, Days, Years, Unconfined aquifer, Confined aquifer, Confining bed, Centuries, and Millennia .The Water Cycle: Groundwater Discharge .There's more water than just what you can see is described in the following way

Explanation:

1.A regional confined aquifer is directly recharged by precipitation in the area where the aquifer crops out, having the same characteristics as an unconfined aquifer, Another source of recharge is the infiltration in the same cropping out area of the runoff born on the hillslopes during rains or snowmelt

2.The pressure in such an aquifer commonly is called artesian pressure, and the formation containing artesian water is an artesian aquifer or confined aquifer. ... --an process where water is put back into ground-water storage from surface-water supplies such as irrigation, or induced infiltration from streams or wells.

3.Groundwater flow lines, which represent the paths of groundwater downslope, are drawn perpendicular to the contour lines. ... Remember: groundwater always moves from an area of higher hydraulic head to an area of lower hydraulic head, and perpendicular to equipotential lines.

4.Groundwater flow lines, which represent the paths of groundwater downslope, are drawn perpendicular to the contour lines. ... Remember: groundwater always moves from an area of higher hydraulic head to an area of lower hydraulic head, and perpendicular to equipotential lines.

5.After entering an aquifer, water moves slowly toward lower lying places and eventually is discharged from the aquifer from springs, seeps into streams, or is withdrawn from the ground by wells. Groundwater in aquifers between layers of poorly permeable rock, such as clay or shale, may be confined under pressure.

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