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if the 2nd half of the 20th century has taught us anything, it is that there are not many phenomena in the world with the characteristics to drastically alter the dynamics of civilizations. we have seen many efforts to alter the climate that were not effective. we do not know how effective mankind will be at co2 removal if they are afforded the tools of civilization. the jury is still out on this question.

factors that contribute to the progressive burial of organic layers include the 1) convective outflow, 2) deep drainage, 3) subglacial hydrologic processes, 4) tectonic activity, and 5) climate change. climate change contributes to both burial and the risk of carbon release.

snowmelt runoff is vital to a stream’s supply and transport processes. however, also causes runoff flooding, sediment deposition, and loss of plant and animal life. fluvial sediment also changes the chemical compositions of stream sediments. often, the combination of these changes leads to dead zones. in some cases, chemicals that were carried in the water can stay in the water after the water has gone through the stream. these chemicals can be dangerous.

the chemical composition of a stream determines its ability to support aquatic life. the presence of phosphate, for example, is essential to plant and animal life. however, phosphate levels in many streams are low, and this is changing. phosphate levels are falling in the united states, europe, and asia.

cycling hypoxia, also called eutrophication, is caused by the over-enrichment of a stream with nutrients (especially nitrogen and phosphorus). this enrichment causes the conversion of surface sediment to turbid, oxygen-depleted sediments which are no longer suitable to support aquatic life. cycling hypoxia often leads to algal blooms and fish kills. it also leads to eutrophic stagnation (es) or oxygen-deficient habitat (odh) where concentrations of oxygen in streams are depleted to 3 mg/l or lower over periods of days to weeks.

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