![]() ![]() ![]() If surface water enters the aquifer near a spring, the water can move quickly through the aquifer and discharge at the spring vent. In Florida, many surface waters contain natural tannic acids from organic material in subsurface rocks, and the color from these streams can appear in springs. Its red iron coloring and metals enrichment are caused by groundwater coming in contact with naturally occurring minerals present as a result of ancient volcanic activity in the area. Water from some springs, however, may be "tea-colored." This picture shows a natural spring in southwestern Colorado. Water from springs usually is remarkably clear. But, as this picture of the wall of the Grand Canyon in Arizona shows, springs can occur when geologic, hydrologic, or human forces cut into the underground layers of soil and rock where water is in movement. ![]() Most people probably think of a spring as being like a pool of water-and normally that is the case. Human activities also can influence the volume of water that discharges from a spring-groundwater withdrawals in an area can cause water levels in the aquifer system to drop and ultimately decreasing the flow from the spring. The amount of water that flows from springs depends on many factors, including the size of the caverns within the rocks, the water pressure in the aquifer, the size of the spring basin, and the amount of rainfall. This process often takes tens to hundreds of thousands of years to complete. As the process continues, the water hollows out more rock, eventually admitting an airspace, at which point the spring stream can be considered a cave. #Silver screen video hot springs ar crack#When it reaches a horizontal crack or a layer of non-dissolving rock such as sandstone or shale, it begins to cut sideways. When weak carbonic acid (formed by rainwater percolating through organic matter in the soil) enters these fractures it dissolves bedrock. Both dolomite and limestone fracture relatively easily. In Missouri, the largest springs are formed in limestone and dolomite in the karst topography of the Ozarks. ![]() Springs may be formed in any sort of rock. They range in size from intermittent seeps, which flow only after much rain, to huge pools flowing hundreds of millions of gallons daily. A spring is the result of an aquifer being filled to the point that the water overflows onto the land surface. Rainbow Springs, Florida, USAA spring is a water resource formed when the side of a hill, a valley bottom or other excavation intersects a flowing body of groundwater at or below the local water table, below which the subsurface material is saturated with water. The hot water (over 300 degrees Celsius) coming from these springs is also rich in minerals and sulfur, which results in a unique ecosystem where unusual and exotic sea life seems to thrive. Recently, scientists have discovered hot springs at depths of up to 2.5 kilometers in the oceans, generally along mid-ocean rifts (spreading ridges). Springs are not limited to the Earth's surface, though. A spring is a water resource formed when the side of a hill, a valley bottom or other excavation intersects a flowing body of groundwater at or below the local water table, below which the subsurface material is saturated with water. ![]()
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