Springs may be formed in any sort of rock. Small ones are found in many places. In Missouri, the largest springs are formed in limestone and dolomite in the karst topography of the Ozarks. Both dolomite and limestone fracture relatively easily. When weak carbonic acid (formed by rainwater percolating through organic matter in the soil) enters these fractures it dissolves bedrock. When it reaches a horizontal crack or a layer of non-dissolving rock such as sandstone or shale, it begins to cut sideways. 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. This process often takes tens to hundreds of thousands of years to complete.
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A. Every interior wall, floor, ceiling, and cabinet shall be maintained in a clean, sanitary, safe, and structurally sound condition, free of large holes and serious cracks, loose plaster or wallpaper, flaking, peeling or scaling paint.
When some places are in a drought, they may be dry, hot and dusty; cracks may appear in the soil, and rivers, lakes, streams, and other sources of water may go dry. Other places in drought get some rain, but not as much as they usually receive during that season. A drought means that a place has less precipitation (rain or snow) than normal over a few months or even longer.
Many macaws have vibrant plumage. The coloring is suited to life in Central and South American rain forests, with their green canopies and colorful fruits and flowers. The birds boast large, powerful beaks that easily crack nuts and seeds, while their dry, scaly tongues have a bone inside them that makes them an effective tool for tapping into fruits.
Here is no water but only rockRock and no water and the sandy roadThe road winding above among the mountainsWhich are mountains of rock without waterIf there were water we should stop and drinkAmongst the rock one cannot stop or thinkSweat is dry and feet are in the sandIf there were only water amongst the rockDead mountain mouth of carious teeth that cannot spitHere one can neither stand nor lie nor sitThere is not even silence in the mountainsBut dry sterile thunder without rainThere is not even solitude in the mountainsBut red sullen faces sneer and snarlFrom doors of mud-cracked housesIf there were waterAnd no rockIf there were rockAnd also waterAnd waterA springA pool among the rockIf there were the sound of water onlyNot the cicadaAnd dry grass singingBut sound of water over a rockWhere the hermit-thrush sings in the pine treesDrip drop drip drop drop drop dropBut there is no water
A damp basement, or any other structure, is often caused by moisture condensation from humid air onto cooler surfaces. Excessive moisture may indicate that repairs or additional insulation are needed. Replace cracked or defective mortar. Some basements are continually wet from water leaking through crevices in the wall. Make sure outside drainage is adequate.
Paper and booksRemove any dry, loose mold from paper with a clean, soft cloth. If mildewed paper is damp, dry it first in an airy place. To dry wallpaper, heat the room for several hours or even days to dry the plaster as well as the paper. Plaster should be dried slowly to prevent cracking. 2ff7e9595c
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