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Sand forms over millions of years through the gradual breakdown of rocks by weathering, erosion, and transportation. Weathering occurs in two primary forms: physical (mechanical) weathering, where temperature changes, wind, water, and glaciers break rocks apart without altering their composition, and chemical weathering, where reactions like hydrolysis, oxidation, and dissolution weaken minerals, making them more susceptible to fragmentation. Once broken down, these particles are transported by rivers, glaciers, wind, and ocean currents, which further shape and refine them. Over time, they are deposited in various environments, leading to different types of sand, such as desert sand (fine and wind-polished), beach sand (smooth and rounded by waves), river sand (coarser and mixed with other sediments), and volcanic sand (dark, mineral-rich, and derived from basalt). The most common mineral in sand is quartz due to its high resistance to weathering, though other minerals and biological materials like feldspar, mica, coral, and shell fragments can contribute to its composition. As sand accumulates, natural forces continue sorting and refining it, gradually removing weaker minerals and leaving behind more uniform grains. This ongoing cycle of rock breakdown, transport, and deposition shapes landscapes across the world, forming the beaches, deserts, and riverbeds we see today. #timdillon #podcasts #timdillonpodcast #comedy #hopecore #hopelesscore #standup #standupcomedy #nature #trump #danawhite #ufc #alexjones #kanye #natureisbetteronline #usa #maga #joeydiaz #actionbronson