KnowraSilicate weatheringLinked fromLinked fromThe 11 pages that link to Silicate weathering, each with the reason it gives.All 11Broader topic 1Related 9Narrower topic 1Silicate mineralRelated: Its rates affect carbon dioxide removal and climate over geological timescales.Snowball EarthRelated: Its climate-cooling effect weakens when ice restricts rainfall and exposed rock.Paleocene–Eocene Thermal MaximumRelated: Enhanced weathering helped remove excess carbon and restore climate over millennia.Carbon mineralizationRelated: Weathering supplies calcium and magnesium that can combine with dissolved carbon dioxide.Carbonate–silicate cycleRelated: It consumes atmospheric carbon dioxide and supplies dissolved material that can become carbonate rock.Huronian glaciationRelated: Reduced weathering under ice could allow volcanic carbon dioxide to accumulate and promote deglaciation.Sturtian glaciationRelated: Enhanced weathering before the ice age may have lowered atmospheric carbon dioxide and cooled the planet.Marinoan glaciationRelated: Its suppression during widespread glaciation is one proposed route to atmospheric carbon dioxide buildup.FayaliteNarrower topic: Fayalite alters through weathering reactions that release iron and silica.Late Paleozoic icehouseRelated: Enhanced weathering during mountain building could have helped draw down greenhouse gases.Dissolved loadBroader topic: Its dissolved products are transported by rivers and affect long-term carbon cycling.