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River
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<h2 id="topography">Topography</h2> <h3>Definition</h3> <p>A river is a natural flow of <a href="/facts/Fresh_water/xMP2TxwI">freshwater</a> that flows on or through <a href="/facts/Land/sYfevlh5">land</a> towards another body of water downhill.<a class="footnote-ref" id="fnref:1" href="#fn:1"><sup>1</sup></a> This flow can be into a <a href="/facts/Lake/YP0xxn0E">lake</a>, an <a href="/facts/Ocean/8W8lYgjD">ocean</a>, or another river.<a class="footnote-ref" id="fnref:2" href="#fn:2"><sup>2</sup></a> A <a href="/facts/Stream/S5he7Cuo">stream</a> refers to water that flows in a natural <a href="/facts/Channel_(geography)/zanMS2Ek">channel</a>, a geographic feature that can contain flowing water.<a class="footnote-ref" id="fnref:3" href="#fn:3"><sup>3</sup></a> A stream may also be referred to as a watercourse.<a class="footnote-ref" id="fnref:4" href="#fn:4"><sup>4</sup></a> The study of the movement of water as it occurs on Earth is called <a href="/facts/Hydrology/Xh727cnE">hydrology</a>, and their effect on the landscape is covered by <a href="/facts/Geomorphology/MDf2I2h5">geomorphology</a>.<a class="footnote-ref" id="fnref:5" href="#fn:5"><sup>5</sup></a> </p> <h3>Source and drainage basin</h3> <p>Rivers are part of the <a href="/facts/Water_cycle/wALHdKjJ">water cycle</a>, the continuous processes by which <a href="/facts/Water/0lkXnJPK">water</a> moves about Earth.<a class="footnote-ref" id="fnref:6" href="#fn:6"><sup>6</sup></a> This means that all water that flows in rivers must ultimately come from <a href="/facts/Precipitation/uq3nGQc8">precipitation</a>.<a class="footnote-ref" id="fnref:7" href="#fn:7"><sup>7</sup></a> The sides of rivers have land that is at a higher <a href="/facts/Elevation/h2d0u9nd">elevation</a> than the river itself, and in these areas, water flows downhill into the river.<a class="footnote-ref" id="fnref:8" href="#fn:8"><sup>8</sup></a> The <a href="/facts/Headwaters/08NFsHeG">headwaters</a> of a river are the smaller <a href="/facts/Streams/MWSDgwBL">streams</a> that feed a river, and make up the river's source.<a class="footnote-ref" id="fnref:9" href="#fn:9"><sup>9</sup></a> These streams may be small and flow rapidly down the sides of <a href="/facts/Mountains/wboT5GJc">mountains</a>.<a class="footnote-ref" id="fnref:10" href="#fn:10"><sup>10</sup></a> All of the <a href="/facts/Land/sYfevlh5">land</a> uphill of a river that feeds it with water in this way is in that river's <a href="/facts/Drainage_basin/lzsx0XJS">drainage basin</a> or watershed.<a class="footnote-ref" id="fnref:11" href="#fn:11"><sup>11</sup></a> A <a href="/facts/Ridge/vd9Waeml">ridge</a> of higher elevation land is what typically separates drainage basins; water on one side of a ridge will flow into one set of rivers, and water on the other side will flow into another.<a class="footnote-ref" id="fnref:12" href="#fn:12"><sup>12</sup></a> One example of this is the <a href="/facts/Continental_Divide_of_the_Americas/BkSDplrg">Continental Divide of the Americas</a> in the <a href="/facts/Rocky_Mountains/rDc3cU0E">Rocky Mountains</a>. Water on the western side of the divide flows into the <a href="/facts/Pacific_Ocean/bdxgXRVM">Pacific Ocean</a>, whereas water on the other side flows into the <a href="/facts/Atlantic_Ocean/EI4uChIb">Atlantic Ocean</a>.<a class="footnote-ref" id="fnref:13" href="#fn:13"><sup>13</sup></a> </p> <p>Not all precipitation flows directly into rivers; some water seeps into underground <a href="/facts/Aquifers/UwG6ksdG">aquifers</a>.<a class="footnote-ref" id="fnref:14" href="#fn:14"><sup>14</sup></a> These, in turn, can still feed rivers via the <a href="/facts/Water_table/2j0VD0lF">water table</a>, the <a href="/facts/Groundwater/JYM2IDS2">groundwater</a> beneath the surface of the land stored in the <a href="/facts/Soil/5Ddpr3QM">soil</a>. Water flows into rivers in places where the river's elevation is lower than that of the water table.<a class="footnote-ref" id="fnref:15" href="#fn:15"><sup>15</sup></a> This phenomenon is why rivers can still flow even during times of <a href="/facts/Drought/LVW0rfuV">drought</a>.<a class="footnote-ref" id="fnref:16" href="#fn:16"><sup>16</sup></a> Rivers are also fed by the melting of <a href="/facts/Snow/HEFKcgIB">snow</a> <a href="/facts/Glaciers/8GrKVUSS">glaciers</a> present in higher elevation regions.<a class="footnote-ref" id="fnref:17" href="#fn:17"><sup>17</sup></a> In <a href="/facts/Summer/v3DY22Uq">summer</a> months, higher temperatures melt snow and ice, causing additional water to flow into rivers. Glacier melt can supplement snow melt in times like the late summer, when there may be less snow left to melt, helping to ensure that the rivers downstream of the glaciers have a continuous supply of water.<a class="footnote-ref" id="fnref:18" href="#fn:18"><sup>18</sup></a> </p> <h3>The flow of rivers</h3> <p>Rivers flow downhill, with their direction determined by <a href="/facts/Gravity/bqAN7DdQ">gravity</a>.<a class="footnote-ref" id="fnref:19" href="#fn:19"><sup>19</sup></a> A <a href="/facts/Common_misconception/rxSqIHvF">common misconception</a> holds that all or most rivers flow from North to South, but this is not true.<a class="footnote-ref" id="fnref:20" href="#fn:20"><sup>20</sup></a> As rivers flow downstream, they eventually merge to form larger rivers. A river that feeds into another is a <a href="/facts/Tributary/JB69Ypox">tributary</a>, and the place they meet is a <a href="/facts/Confluence/3ygntlsh">confluence</a>.<a class="footnote-ref" id="fnref:21" href="#fn:21"><sup>21</sup></a> Rivers must flow to lower altitudes due to <a href="/facts/Gravity/bqAN7DdQ">gravity</a>.<a class="footnote-ref" id="fnref:22" href="#fn:22"><sup>22</sup></a> The <a href="/facts/Stream_bed/9hcQPGaj">bed</a> of a river is typically within a <a href="/facts/River_valley/gKmvE6L1">river valley</a> between <a href="/facts/Hills/wnUG3lUL">hills</a> or <a href="/facts/Mountains/wboT5GJc">mountains</a>. Rivers flowing through an <a href="/facts/Permeability_(materials_science)/ja7dRwgU">impermeable</a> section of land such as rocks will <a href="/facts/Erosion/gaGJXy0W">erode</a> the slopes on the sides of the river.<a class="footnote-ref" id="fnref:23" href="#fn:23"><sup>23</sup></a> When a river carves a <a href="/facts/Plateau/RtbmsmfB">plateau</a> or a similar high-elevation area, a <a href="/facts/Canyon/YspSIEz3">canyon</a> can form, with cliffs on either side of the river.<a class="footnote-ref" id="fnref:24" href="#fn:24"><sup>24</sup></a><a class="footnote-ref" id="fnref:25" href="#fn:25"><sup>25</sup></a> Areas of a river with softer rock <a href="/facts/Weathering/uSYGlv0H">weather</a> faster than areas with harder rock, causing a difference in elevation between two points of a river. This can cause the formation of a <a href="/facts/Waterfall/CDyaLQIQ">waterfall</a> as the river's flow falls down a vertical drop.<a class="footnote-ref" id="fnref:26" href="#fn:26"><sup>26</sup></a> </p> <p>A river in a permeable area does not exhibit this behavior and may even have raised <a href="/facts/Bank_(geography)/sQkkIEkd">banks</a> due to sediment.<a class="footnote-ref" id="fnref:27" href="#fn:27"><sup>27</sup></a> Rivers also change their landscape through their transportation of <a href="/facts/Sediment/zsIH1A6U">sediment</a>, often known as <a href="/facts/Alluvium/Bo78QRlp">alluvium</a> when applied specifically to rivers.<a class="footnote-ref" id="fnref:28" href="#fn:28"><sup>28</sup></a><a class="footnote-ref" id="fnref:29" href="#fn:29"><sup>29</sup></a> This debris comes from erosion performed by the rivers themselves, debris swept into rivers by rainfall, as well as erosion caused by the slow movement of glaciers. The sand in deserts and the sediment that forms bar islands is from rivers.<a class="footnote-ref" id="fnref:30" href="#fn:30"><sup>30</sup></a> The <a href="/facts/Particle_size/KWwwGkn4">particle size</a> of the debris is gradually sorted by the river, with heavier particles like <a href="/facts/Rocks/FXCJkmop">rocks</a> sinking to the bottom, and finer particles like <a href="/facts/Sand/MdTIt0M8">sand</a> or <a href="/facts/Silt/HAxJkhDP">silt</a> carried further <a href="/facts/Current_(hydrology)/xRdgYLdU">downriver</a>. This sediment may be deposited in river valleys or carried to the <a href="/facts/Sea/7eo8zrRW">sea</a>.<a class="footnote-ref" id="fnref:31" href="#fn:31"><sup>31</sup></a> </p><p>The sediment yield of a river is the quantity of sand per unit area within a watershed that is removed over a period of time.<a class="footnote-ref" id="fnref:32" href="#fn:32"><sup>32</sup></a> The monitoring of the sediment yield of a river is important for ecologists to understand the health of its ecosystems, the rate of erosion of the river's environment, and the effects of human activity.<a class="footnote-ref" id="fnref:33" href="#fn:33"><sup>33</sup></a> </p> <p>Rivers rarely run in a straight direction, instead preferring to bend or <a href="/facts/Meander/XIGCmCq9">meander</a>.<a class="footnote-ref" id="fnref:34" href="#fn:34"><sup>34</sup></a> This is because any natural impediment to the flow of the river may cause the current to deflect in a different direction. When this happens, the alluvium carried by the river can build up against this impediment, redirecting the course of the river. The flow is then directed against the opposite bank of the river, which will erode into a more concave shape to accommodate the flow. The bank will still block the flow, causing it to reflect in the other direction. Thus, a bend in the river is created.<a class="footnote-ref" id="fnref:35" href="#fn:35"><sup>35</sup></a> </p><p>Rivers may run through low, flat regions on their way to the sea.<a class="footnote-ref" id="fnref:36" href="#fn:36"><sup>36</sup></a> These places may have <a href="/facts/Floodplains/EUKqIbj5">floodplains</a> that are periodically flooded when there is a high level of water running through the river. These events may be referred to as "wet seasons' and "dry seasons" when the flooding is predictable due to the <a href="/facts/Climate/f57XrNFU">climate</a>.<a class="footnote-ref" id="fnref:37" href="#fn:37"><sup>37</sup></a> The alluvium carried by rivers, laden with minerals, is deposited into the floodplain when the banks spill over, providing new nutrients to the soil, allowing them to support human activity like farming as well as a host of plant and animal life.<a class="footnote-ref" id="fnref:38" href="#fn:38"><sup>38</sup></a><a class="footnote-ref" id="fnref:39" href="#fn:39"><sup>39</sup></a> Deposited sediment from rivers can form temporary or long-lasting <a href="/facts/River_island/B0RJRqdI">fluvial islands</a>.<a class="footnote-ref" id="fnref:40" href="#fn:40"><sup>40</sup></a> These islands exist in almost every river.<a class="footnote-ref" id="fnref:41" href="#fn:41"><sup>41</sup></a> </p> <h4>Non-perennial rivers</h4> <p>About half of all waterways on Earth are <a href="/facts/Intermittent_rivers/UIPqg1S7">intermittent rivers</a>, which do not always have a continuous flow of water throughout the year.<a class="footnote-ref" id="fnref:42" href="#fn:42"><sup>42</sup></a> This may be because an arid climate is too dry depending on the season to support a stream, or because a river is seasonally frozen in the winter (such as in an area with substantial <a href="/facts/Permafrost/SkFC7LMT">permafrost</a>), or in the headwaters of rivers in mountains, where <a href="/facts/Snowmelt/GHknH4bQ">snowmelt</a> is required to fuel the river.<a class="footnote-ref" id="fnref:43" href="#fn:43"><sup>43</sup></a> These rivers can appear in a variety of climates, and still provide a habitat for aquatic life and perform other ecological functions.<a class="footnote-ref" id="fnref:44" href="#fn:44"><sup>44</sup></a> </p> <h4>Subterranean rivers</h4> <p><a href="/facts/Subterranean_river/qMy9L50M">Subterranean rivers</a> may flow underground through flooded caves.<a class="footnote-ref" id="fnref:45" href="#fn:45"><sup>45</sup></a> This can happen in <a href="/facts/Karst/IzJYhjVN">karst</a> systems, where rock dissolves to form caves. These rivers provide a habitat for diverse <a href="/facts/Microorganisms/pysJYcE2">microorganisms</a> and have become an important target of study by <a href="/facts/Microbiologists/cqEyJwNK">microbiologists</a>.<a class="footnote-ref" id="fnref:46" href="#fn:46"><sup>46</sup></a> Other rivers and streams have been covered over or converted to run in tunnels due to human development.<a class="footnote-ref" id="fnref:47" href="#fn:47"><sup>47</sup></a> These rivers do not typically host any life, and are often used only for <a href="/facts/Stormwater/CX4EcIWu">stormwater</a> or flood control.<a class="footnote-ref" id="fnref:48" href="#fn:48"><sup>48</sup></a> One such example is the <a href="/facts/Sunswick_Creek/4aNWM0bs">Sunswick Creek</a> in New York City, which was covered in the 1800s and now exists only as a sewer-like pipe.<a class="footnote-ref" id="fnref:49" href="#fn:49"><sup>49</sup></a> </p> <h3>The terminus</h3> <p>While rivers may flow into <a href="/facts/Lakes/YP0xxn0E">lakes</a> or man-made features such as <a href="/facts/Reservoirs/2FewszmR">reservoirs</a>, the water they contain will always tend to flow down toward the <a href="/facts/Ocean/8W8lYgjD">ocean</a>.<a class="footnote-ref" id="fnref:50" href="#fn:50"><sup>50</sup></a> However, if human activity siphons too much water away from a river for other uses, the riverbed may run dry before reaching the sea.<a class="footnote-ref" id="fnref:51" href="#fn:51"><sup>51</sup></a> The outlets <a href="/facts/River_mouth/qxKhJCVP">mouth</a> of a river can take several forms. <a href="/facts/Tidal_river/olDupr2s">Tidal rivers</a> (often part of an <a href="/facts/Estuary/WmkSInmK">estuary</a>) have their levels rise and fall with the <a href="/facts/Tide/zNstvWPv">tide</a>.<a class="footnote-ref" id="fnref:52" href="#fn:52"><sup>52</sup></a> Since the levels of these rivers are often already at or near sea level, the flow of alluvium and the <a href="/facts/Brackish_water/f6z3UXCa">brackish water</a> that flows in these rivers may be either <a href="/facts/Upriver/xRdgYLdU">upriver</a> or downriver depending on the time of day.<a class="footnote-ref" id="fnref:53" href="#fn:53"><sup>53</sup></a> </p><p>Rivers that are not tidal may form <a href="/facts/Deltas/fmWuaRqX">deltas</a> that continuously deposit alluvium into the sea from their mouths.<a class="footnote-ref" id="fnref:54" href="#fn:54"><sup>54</sup></a> Depending on the activity of waves, the strength of the river, and the strength of the tidal current, the sediment can accumulate to form new land.<a class="footnote-ref" id="fnref:55" href="#fn:55"><sup>55</sup></a> When viewed from above, a delta can appear to take the form of several <a href="/facts/Triangular/cRXUwsMn">triangular</a> shapes as the river mouth appears to fan out from the original <a href="/facts/Coastline/RBD0wxn3">coastline</a>.<a class="footnote-ref" id="fnref:56" href="#fn:56"><sup>56</sup></a> </p> <h2 id="classification">Classification</h2> <p class="note">Main article: <a href="/facts/Stream_order/sBvhp4wN">Stream order</a></p> <p>In <a href="/facts/Hydrology/Xh727cnE">hydrology</a>, a stream order is a positive integer used to describe the level of river branching in a drainage basin.<a class="footnote-ref" id="fnref:57" href="#fn:57"><sup>57</sup></a> Several systems of stream order exist, one of which is the <a href="/facts/Strahler_number/NvIPLc2u">Strahler number</a>. In this system, the first tributaries of a river are 1st order rivers. When two 1st order rivers merge, the resulting river is 2nd order. If a river of a higher order and a lower order merge, the order is incremented from whichever of the previous rivers had the higher order.<a class="footnote-ref" id="fnref:58" href="#fn:58"><sup>58</sup></a> Stream order is correlated with and thus can be used to predict certain data points related to rivers, such as the size of the drainage basin (drainage area), and the length of the channel.<a class="footnote-ref" id="fnref:59" href="#fn:59"><sup>59</sup></a> </p> <h2 id="ecology">Ecology</h2> <h3>Models</h3> <h4>River Continuum Concept</h4> <p>The <a href="/facts/River_ecosystem/qY1TgRuM">ecosystem of a river</a> includes the life that lives in its water, on its banks, and in the surrounding land.<a class="footnote-ref" id="fnref:60" href="#fn:60"><sup>60</sup></a> The width of the channel of a river, its velocity, and how shaded it is by nearby trees. Creatures in a river ecosystem may be divided into many roles based on the <a href="/facts/River_Continuum_Concept/XXbe7a1l">River Continuum Concept</a>. "Shredders" are organisms that consume this organic material. The role of a "grazer" or "scraper" organism is to feed on the <a href="/facts/Algae/U1ftVKU3">algae</a> that collects on rocks and plants. "Collectors" consume the <a href="/facts/Detritus/8IjhrXA6">detritus</a> of dead organisms. Lastly, <a href="/facts/Predators/JEGdrX3f">predators</a> feed on living things to survive.<a class="footnote-ref" id="fnref:61" href="#fn:61"><sup>61</sup></a> </p><p>The river can then be modeled by the availability of resources for each creature's role. A shady area with <a href="/facts/Deciduous/7jQHVtdd">deciduous</a> trees might experience frequent deposits of <a href="/facts/Organic_matter/t17tVCvk">organic matter</a> in the form of leaves. In this type of ecosystem, collectors and shredders will be most active.<a class="footnote-ref" id="fnref:62" href="#fn:62"><sup>62</sup></a> As the river becomes deeper and wider, it may move slower and receive more <a href="/facts/Sunlight/WPkJRC7s">sunlight</a>. This supports <a href="/facts/Invertebrates/3CyqCVnN">invertebrates</a> and a variety of <a href="/facts/Fish/fln4gH9V">fish</a>, as well as scrapers feeding on algae.<a class="footnote-ref" id="fnref:63" href="#fn:63"><sup>63</sup></a> Further downstream, the river may get most of its energy from organic matter that was already processed upstream by collectors and shredders. Predators may be more active here, including fish that feed on plants, <a href="/facts/Plankton/WGo3LU9T">plankton</a>, and other fish.<a class="footnote-ref" id="fnref:64" href="#fn:64"><sup>64</sup></a> </p> <h4>Flood pulse concept</h4> <p>The <a href="/facts/Flood_pulse_concept/YzQT0MIx">flood pulse concept</a> focuses on habitats that flood seasonally, including <a href="/facts/Lakes/YP0xxn0E">lakes</a> and <a href="/facts/Marshes/AG0WLJ2K">marshes</a>. The land that interfaces with a water body is that body's <a href="/facts/Riparian_zone/3NQHWM78">riparian zone</a>. Plants in the riparian zone of a river help stabilize its banks to prevent erosion and filter alluvium deposited by the river on the shore, including processing the <a href="/facts/Nitrogen/Nf1QpGDz">nitrogen</a> and other nutrients it contains. Forests in a riparian zone also provide important animal <a href="/facts/Habitats/zo1DN2gA">habitats</a>.<a class="footnote-ref" id="fnref:65" href="#fn:65"><sup>65</sup></a> </p> <h4>Fish zonation concept</h4> <p>River ecosystems have also been categorized based on the variety of aquatic life they can sustain, also known as the fish zonation concept.<a class="footnote-ref" id="fnref:66" href="#fn:66"><sup>66</sup></a> Smaller rivers can only sustain smaller fish that can comfortably fit in its waters, whereas larger rivers can contain both small fish and large fish. This means that larger rivers can host a larger variety of species.<a class="footnote-ref" id="fnref:67" href="#fn:67"><sup>67</sup></a> This is analogous to the <a href="/facts/Species-area_relationship/pAowgFT8">species-area relationship</a>, the concept of larger habitats being host to more species. In this case, it is known as the species-discharge relationship, referring specifically to the <a href="/facts/Discharge_regime/XwpV8U8K">discharge</a> of a river, the amount of water passing through it at a particular time.<a class="footnote-ref" id="fnref:68" href="#fn:68"><sup>68</sup></a> </p> <h3>Movement of organisms</h3> <p>The flow of a river can act as a means of transportation for different organisms, as well as a barrier. For example, the <a href="/facts/Amazon_River/Ha9AzJY5">Amazon River</a> is so wide in parts that the variety of species on either side of its <a href="/facts/Amazon_basin/kVk5XeHA">basin</a> are distinct.<a class="footnote-ref" id="fnref:69" href="#fn:69"><sup>69</sup></a> Some <a href="/facts/Fish/fln4gH9V">fish</a> may swim upstream to <a href="/facts/Spawn_(biology)/nYF12vfX">spawn</a> as part of a seasonal <a href="/facts/Fish_migration/obNpLAUD">migration</a>. Species that travel from the <a href="/facts/Sea/7eo8zrRW">sea</a> to breed in <a href="/facts/Freshwater/xMP2TxwI">freshwater</a> rivers are <a href="/facts/Fish_migration/obNpLAUD">anadromous</a>, and fish that travel from rivers to the <a href="/facts/Ocean/8W8lYgjD">ocean</a> to breed are <a href="/facts/Fish_migration/obNpLAUD">catadromous</a>. <a href="/facts/Salmon/7kUsoqVN">Salmons</a> are anadromous fish that may die in the river after spawning, contributing <a href="/facts/Nutrient_cycle/S57nuGbQ">nutrients</a> back to the <a href="/facts/River_ecosystem/qY1TgRuM">river ecosystem</a>.<a class="footnote-ref" id="fnref:70" href="#fn:70"><sup>70</sup></a> <a href="/facts/Fungus/BHo5DP59">Fungal</a> spores also sometimes move via stream currents, and some species depend on this to spread between substrates.<a class="footnote-ref" id="fnref:71" href="#fn:71"><sup>71</sup></a> </p> <h2 id="human-uses">Human uses</h2> <h3>Infrastructure</h3> <p class="note">Main article: <a href="/facts/River_engineering/jLfX5fJ4">River engineering</a></p> <p>Modern river engineering involves a large-scale collection of independent river engineering structures that have the goal of <a href="/facts/Flood_control/rf0476SJ">flood control</a>, improved navigation, recreation, and ecosystem management.<a class="footnote-ref" id="fnref:72" href="#fn:72"><sup>72</sup></a> Many of these projects have the effect of normalizing the effects of rivers; the greatest floods are smaller and more predictable, and larger sections are open for navigation by boats and other watercraft.<a class="footnote-ref" id="fnref:73" href="#fn:73"><sup>73</sup></a> A major effect of river engineering has been a reduced sediment output of large rivers. For example, the <a href="/facts/Mississippi_River/RduarPzj">Mississippi River</a> produced 400 million tons of sediment per year.<a class="footnote-ref" id="fnref:74" href="#fn:74"><sup>74</sup></a> Due to the construction of <a href="/facts/Reservoirs/2FewszmR">reservoirs</a>, sediment buildup in man-made <a href="/facts/Levees/99xdvoVg">levees</a>, and the removal of natural banks replaced with <a href="/facts/Revetments/xGIP8crD">revetments</a>, this sediment output has been reduced by 60%.<a class="footnote-ref" id="fnref:75" href="#fn:75"><sup>75</sup></a> </p><p>The most basic river projects involve the clearing of obstructions like fallen trees. This can scale up to <a href="/facts/Dredging/81sUKhnF">dredging</a>, the excavation of sediment buildup in a channel, to provide a deeper area for navigation.<a class="footnote-ref" id="fnref:76" href="#fn:76"><sup>76</sup></a> These activities require regular maintenance as the location of the river banks changes over time, floods bring foreign objects into the river, and natural sediment buildup continues.<a class="footnote-ref" id="fnref:77" href="#fn:77"><sup>77</sup></a> Artificial <a href="/facts/Channel_(geography)/zanMS2Ek">channels</a> are often constructed to "cut off" winding sections of a river with a shorter path, or to direct the flow of a river in a straighter direction.<a class="footnote-ref" id="fnref:78" href="#fn:78"><sup>78</sup></a> This effect, known as channelization, has made the distance required to traverse the <a href="/facts/Missouri_River/NL8Sj9Wb">Missouri River</a> in 116 kilometres (72 mi) shorter.<a class="footnote-ref" id="fnref:79" href="#fn:79"><sup>79</sup></a> </p> <p>Dikes are channels built perpendicular to the flow of the river beneath its surface. These help rivers flow straighter by increasing the speed of the water at the middle of the channel, helping to control floods.<a class="footnote-ref" id="fnref:80" href="#fn:80"><sup>80</sup></a> Levees are also used for this purpose. They can be thought of as dams constructed on the sides of rivers, meant to hold back water from flooding the surrounding area during periods of high rainfall. They are often constructed by building up the natural terrain with soil or clay.<a class="footnote-ref" id="fnref:81" href="#fn:81"><sup>81</sup></a> Some levees are supplemented with floodways, channels used to redirect floodwater away from farms and populated areas.<a class="footnote-ref" id="fnref:82" href="#fn:82"><sup>82</sup></a> </p><p><a href="/facts/Dams/BroJFhEI">Dams</a> restrict the flow of water through a river. They can be built for navigational purposes, providing a higher level of water upstream for boats to travel in. They may also be used for <a href="/facts/Hydroelectricity/zEeJIK2B">hydroelectricity</a>, or power generation from rivers.<a class="footnote-ref" id="fnref:83" href="#fn:83"><sup>83</sup></a> Dams typically transform a section of the river behind them into a lake or reservoir. This can provide nearby cities with a predictable supply of drinking water. Hydroelectricity is desirable as a form of <a href="/facts/Renewable_energy/6Bu6IrpF">renewable energy</a> that does not require any inputs beyond the river itself.<a class="footnote-ref" id="fnref:84" href="#fn:84"><sup>84</sup></a> Dams are very common worldwide, with at least 75,000 higher than 6 feet (1.8 m) in the U.S. Globally, reservoirs created by dams cover 193,500 square miles (501,000 km2).<a class="footnote-ref" id="fnref:85" href="#fn:85"><sup>85</sup></a> Dam-building reached a peak in the 1970s, when between two or three dams were completed every day, and has since begun to decline. New dam projects are primarily focused in <a href="/facts/China/lTjIXY5p">China</a>, <a href="/facts/India/QW4TV4sy">India</a>, and other areas in <a href="/facts/Asia/4IToYrrQ">Asia</a>.<a class="footnote-ref" id="fnref:86" href="#fn:86"><sup>86</sup></a> </p> <h3>History</h3> <h4>Pre-industrial era</h4> <p>The first <a href="/facts/Civilizations/xvGpjDPj">civilizations</a> of Earth were born on floodplains between 5,500 and 3,500 years ago.<a class="footnote-ref" id="fnref:87" href="#fn:87"><sup>87</sup></a> The freshwater, fertile soil, and transportation provided by rivers helped create the conditions for complex societies to emerge. Three such civilizations were the <a href="/facts/Sumerians/bxRz093q">Sumerians</a> in the <a href="/facts/Tigris%25E2%2580%2593Euphrates_river_system/kg6LGEav">Tigris–Euphrates river system</a>, the <a href="/facts/Ancient_Egyptian/BDsEGK4g">Ancient Egyptian</a> civilization in the Nile, and the <a href="/facts/Indus_Valley_Civilization/6xM4aK23">Indus Valley Civilization</a> on the <a href="/facts/Indus_River/7vTRHA4t">Indus River</a>.<a class="footnote-ref" id="fnref:88" href="#fn:88"><sup>88</sup></a><a class="footnote-ref" id="fnref:89" href="#fn:89"><sup>89</sup></a> The <a href="/facts/Desert/Mknp4bXq">desert</a> climates of the surrounding areas made these societies especially reliant on rivers for survival, leading to people clustering in these areas to form the first <a href="/facts/Cities/2uNRFqAN">cities</a>.<a class="footnote-ref" id="fnref:90" href="#fn:90"><sup>90</sup></a> It is also thought that these civilizations were the first to organize the irrigation of desert environments for growing food.<a class="footnote-ref" id="fnref:91" href="#fn:91"><sup>91</sup></a> Growing food at scale allowed people to specialize in other roles, form hierarchies, and organize themselves in new ways, leading to the birth of civilization.<a class="footnote-ref" id="fnref:92" href="#fn:92"><sup>92</sup></a> </p> <p>In <a href="/facts/Pre-industrial_society/hzEubtAQ">pre-industrial society</a>, rivers were a source of transportation and abundant resources.<a class="footnote-ref" id="fnref:93" href="#fn:93"><sup>93</sup></a><a class="footnote-ref" id="fnref:94" href="#fn:94"><sup>94</sup></a> Many civilizations depended on what resources were local to them to survive. <a href="/facts/Shipping/0wYezNsU">Shipping</a> of commodities, especially the floating of <a href="/facts/Wood/z13NpHPl">wood</a> on rivers to transport it, was especially important. Rivers also were an important source of <a href="/facts/Drinking_water/FmSJcKGG">drinking water</a>. For civilizations built around rivers, fish were an important part of the diet of humans.<a class="footnote-ref" id="fnref:95" href="#fn:95"><sup>95</sup></a> Some rivers supported fishing activities, but were ill-suited to farming, such as those in the <a href="/facts/Pacific_Northwest/EjJhETXc">Pacific Northwest</a>.<a class="footnote-ref" id="fnref:96" href="#fn:96"><sup>96</sup></a> Other animals that live in or near rivers like <a href="/facts/Frogs/IxYhbeda">frogs</a>, <a href="/facts/Mussels/SNdrkjfl">mussels</a>, and <a href="/facts/Beavers/uoJ2xU4D">beavers</a> could provide food and valuable goods such as <a href="/facts/Fur/4hVxpDQ0">fur</a>.<a class="footnote-ref" id="fnref:97" href="#fn:97"><sup>97</sup></a> </p><p>Humans have been building <a href="/facts/Infrastructure/QJvbsSpl">infrastructure</a> to use rivers for thousands of years.<a class="footnote-ref" id="fnref:98" href="#fn:98"><sup>98</sup></a> The <a href="/facts/Sadd_el-Kafara/WH3wBqa3">Sadd el-Kafara</a> dam near <a href="/facts/Cairo/dXjj60ar">Cairo</a>, Egypt, is an ancient dam built on the <a href="/facts/Nile/vGoXVUFH">Nile</a> 4,500 years ago. The <a href="/facts/Ancient_Roman/cGqIuxPd">Ancient Roman</a> civilization used aqueducts to transport water to <a href="/facts/Urban_areas/fu9v8h5P">urban areas</a>. <a href="/facts/Spanish_Muslims/rjITCLFj">Spanish Muslims</a> used mills and water wheels beginning in the seventh century. Between 130 and 1492, larger dams were built in Japan, Afghanistan, and India, including 20 dams higher than 15 metres (49 ft).<a class="footnote-ref" id="fnref:99" href="#fn:99"><sup>99</sup></a> Canals began to be cut in Egypt as early as 3000 BC, and the mechanical <a href="/facts/Shadoof/bs2yyDbX">shadoof</a> began to be used to raise the elevation of water.<a class="footnote-ref" id="fnref:100" href="#fn:100"><sup>100</sup></a> Drought years harmed crop yields, and leaders of society were incentivized to ensure regular water and food availability to remain in power. Engineering projects like the shadoof and canals could help prevent these crises.<a class="footnote-ref" id="fnref:101" href="#fn:101"><sup>101</sup></a> Despite this, there is evidence that floodplain-based civilizations may have been abandoned occasionally at a large scale. This has been attributed to unusually large floods destroying infrastructure; however, there is evidence that permanent changes to climate causing higher <a href="/facts/Aridity/BHJj0qJ3">aridity</a> and lower river flow may have been the determining factor in what river civilizations succeeded or dissolved.<a class="footnote-ref" id="fnref:102" href="#fn:102"><sup>102</sup></a> </p> <p><a href="/facts/Water_wheels/7xwQDxrP">Water wheels</a> began to be used at least 2,000 years ago to harness the energy of rivers.<a class="footnote-ref" id="fnref:103" href="#fn:103"><sup>103</sup></a> Water wheels turn an <a href="/facts/Axle/Eo5jWI3f">axle</a> that can supply <a href="/facts/Rotational_energy/sFhMenoK">rotational energy</a> to move water into <a href="/facts/Aqueduct_(water_supply)/jnSsVRYd">aqueducts</a>, work metal using a <a href="/facts/Trip_hammer/SEdYDjtJ">trip hammer</a>, and grind grains with a <a href="/facts/Millstone/q1crPEs4">millstone</a>. In the <a href="/facts/Middle_Ages/RqzEKB9v">Middle Ages</a>, water mills began to automate many aspects of <a href="/facts/Manual_labor/6TTBBCNr">manual labor</a>, and spread rapidly. By 1300, there were at least 10,000 mills in England alone. A medieval watermill could do the work of 30–60 human workers.<a class="footnote-ref" id="fnref:104" href="#fn:104"><sup>104</sup></a> Water mills were often used in conjunction with dams to focus and increase the speed of the water.<a class="footnote-ref" id="fnref:105" href="#fn:105"><sup>105</sup></a> Water wheels continued to be used up to and through the <a href="/facts/Industrial_Revolution/B6E3Fasm">Industrial Revolution</a> as a source of power for <a href="/facts/Textile_mill/Idul45Xb">textile mills</a> and other factories, but were eventually supplanted by <a href="/facts/Steam_power/f7hN8vzm">steam power</a>.<a class="footnote-ref" id="fnref:106" href="#fn:106"><sup>106</sup></a> </p> <h4>Industrial era</h4> <p>Rivers became more <a href="/facts/Industrialized/h3QXzS6C">industrialized</a> with the growth of technology and the <a href="/facts/Human_population/tzYcheuD">human population</a>.<a class="footnote-ref" id="fnref:107" href="#fn:107"><sup>107</sup></a> As fish and water could be brought from elsewhere, and goods and people could be transported via <a href="/facts/Railways/9nJQbsDV">railways</a>, pre-industrial river uses diminished in favor of more complex uses. This meant that the local ecosystems of rivers needed less protection as humans became less reliant on them for their continued flourishing. <a href="/facts/River_engineering/jLfX5fJ4">River engineering</a> began to develop projects that enabled industrial <a href="/facts/Hydropower/Adx1E5ha">hydropower</a>, <a href="/facts/Canals/pBE8LsJx">canals</a> for the more efficient movement of goods, as well as projects for <a href="/facts/Flood_prevention/rf0476SJ">flood prevention</a>.<a class="footnote-ref" id="fnref:108" href="#fn:108"><sup>108</sup></a><a class="footnote-ref" id="fnref:109" href="#fn:109"><sup>109</sup></a> </p><p>River transportation has historically been significantly cheaper and faster than transportation by land.<a class="footnote-ref" id="fnref:110" href="#fn:110"><sup>110</sup></a> Rivers helped fuel <a href="/facts/Urbanization/GQq0oqft">urbanization</a> as goods such as grain and fuel could be floated downriver to supply cities with resources.<a class="footnote-ref" id="fnref:111" href="#fn:111"><sup>111</sup></a> River transportation is also important for the <a href="/facts/Lumber_industry/MysmUzCT">lumber industry</a>, as logs can be shipped via river. Countries with dense forests and networks of rivers like <a href="/facts/Sweden/u3qC7lyj">Sweden</a> have historically benefited the most from this method of trade. The rise of <a href="/facts/Highway/2nxmEmgX">highways</a> and the <a href="/facts/Automobile/I1IsH8IK">automobile</a> has made this practice less common.<a class="footnote-ref" id="fnref:112" href="#fn:112"><sup>112</sup></a> </p> <p>One of the first large canals was the <a href="/facts/Canal_du_Midi/Nq6YRp1N">Canal du Midi</a>, connecting rivers within France to create a path from the <a href="/facts/Atlantic_Ocean/EI4uChIb">Atlantic Ocean</a> to the <a href="/facts/Mediterranean_Sea/Vr2pzVbM">Mediterranean Sea</a>.<a class="footnote-ref" id="fnref:113" href="#fn:113"><sup>113</sup></a> The nineteenth century saw canal-building become more common, with the U.S. building 4,400 miles (7,100 km) of canals by 1830. Rivers began to be used by <a href="/facts/Cargo_ships/G7JSpeMc">cargo ships</a> at a larger scale, and these canals were used in conjunction with river engineering projects like dredging and straightening to ensure the efficient flow of goods.<a class="footnote-ref" id="fnref:114" href="#fn:114"><sup>114</sup></a> One of the largest such projects is that of the <a href="/facts/Mississippi_River/RduarPzj">Mississippi River</a>, whose drainage basin covers 40% of the <a href="/facts/Contiguous_United_States/yx414G7a">contiguous United States</a>. The river was then used for shipping crops from the <a href="/facts/American_Midwest/VanHjkw2">American Midwest</a> and cotton from the <a href="/facts/American_South/ppnGuAtB">American South</a> to other states as well as the Atlantic Ocean.<a class="footnote-ref" id="fnref:115" href="#fn:115"><sup>115</sup></a> </p><p>The role of <a href="/facts/Urban_stream/RxXr2g89">urban rivers</a> has evolved from when they were a center of trade, food, and transportation to modern times when these uses are less necessary.<a class="footnote-ref" id="fnref:116" href="#fn:116"><sup>116</sup></a> Rivers remain central to the <a href="/facts/Cultural_identity/YLUfbbIC">cultural identity</a> of cities and nations. Famous examples include the <a href="/facts/River_Thames/XnQWN52L">River Thames</a>'s relationship to <a href="/facts/London/KozCCsy9">London</a>, the <a href="/facts/Seine/Chd1gSKo">Seine</a> to <a href="/facts/Paris/DrNHpwnA">Paris</a>, and the <a href="/facts/Hudson_River/dGgu7VFE">Hudson River</a> to <a href="/facts/New_York_City/YlyvFmVC">New York City</a>.<a class="footnote-ref" id="fnref:117" href="#fn:117"><sup>117</sup></a> The restoration of water quality and recreation to urban rivers has been a goal of modern administrations. For example, <a href="/facts/Swimming/hnU8XbVg">swimming</a> was banned in the Seine for over 100 years due to concerns about pollution and the spread of <a href="/facts/E._coli/nR4Gvl56">E. coli</a>, until cleanup efforts to allow its use in the <a href="/facts/2024_Summer_Olympics/lo0czN5R">2024 Summer Olympics</a>.<a class="footnote-ref" id="fnref:118" href="#fn:118"><sup>118</sup></a> Another example is the restoration of the <a href="/facts/Isar/REsSPE8T">Isar</a> in <a href="/facts/Munich/Pr6zw2ev">Munich</a> from being a fully canalized channel with hard embankments to being wider with naturally sloped banks and vegetation.<a class="footnote-ref" id="fnref:119" href="#fn:119"><sup>119</sup></a> This has improved wildlife habitat in the Isar, and provided more opportunities for recreation in the river.<a class="footnote-ref" id="fnref:120" href="#fn:120"><sup>120</sup></a> </p> <h3>Politics of rivers</h3> <p class="note">See also: <a href="/facts/Water_rights_law/uFNyJAMn">Water rights law</a></p> <p>As a <a href="/facts/Natural_barrier/gPk2lHpp">natural barrier</a>, rivers are often used as a border between <a href="/facts/Countries/hormuwdR">countries</a>, cities, and other <a href="/facts/Territories/j6KoWv1C">territories</a>.<a class="footnote-ref" id="fnref:121" href="#fn:121"><sup>121</sup></a> For example, the <a href="/facts/Lamari_River/3WV0kmek">Lamari River</a> in <a href="/facts/New_Guinea/qB0bzfSH">New Guinea</a> separates the <a href="/facts/Angu/6YbQ3KIr">Angu</a> and the <a href="/facts/Fore_people/eryCsyed">Fore</a> people in New Guinea. The two cultures speak different languages and rarely mix.<a class="footnote-ref" id="fnref:122" href="#fn:122"><sup>122</sup></a> 23% of international borders are large rivers (defined as those over 30 meters wide).<a class="footnote-ref" id="fnref:123" href="#fn:123"><sup>123</sup></a> The traditional northern border of the <a href="/facts/Roman_Empire/l4E1aUuV">Roman Empire</a> was the <a href="/facts/Danube/8lMeM9xg">Danube</a>, a river that today forms the border of <a href="/facts/Hungary/YRedQLtI">Hungary</a> and <a href="/facts/Slovakia/gmJwpwM3">Slovakia</a>. Since the flow of a river is rarely static, the exact location of a river border may be called into question by countries.<a class="footnote-ref" id="fnref:124" href="#fn:124"><sup>124</sup></a> The <a href="/facts/Rio_Grande/utfAg59u">Rio Grande</a> between the United States and Mexico is regulated by the <a href="/facts/International_Boundary_and_Water_Commission/kTTsxh7G">International Boundary and Water Commission</a> to manage the right to fresh water from the river, as well as mark the exact location of the border.<a class="footnote-ref" id="fnref:125" href="#fn:125"><sup>125</sup></a> </p><p>Up to 60% of fresh water used by countries comes from rivers that cross international borders.<a class="footnote-ref" id="fnref:126" href="#fn:126"><sup>126</sup></a> This can cause disputes between countries that live upstream and downstream of the river. A country that is downstream of another may object to the upstream country diverting too much water for agricultural uses, pollution, as well as the creation of dams that change the river's flow characteristics.<a class="footnote-ref" id="fnref:127" href="#fn:127"><sup>127</sup></a> For example, Egypt has an agreement with <a href="/facts/Sudan/yGeaNdvS">Sudan</a> requiring a specific minimum volume of water to pass into the Nile yearly over the <a href="/facts/Aswan_Dam/6S5TG0Wn">Aswan Dam</a>, to maintain both countries access to water.<a class="footnote-ref" id="fnref:128" href="#fn:128"><sup>128</sup></a> </p> <h3>Religion and mythology</h3> <p class="note">See also: <a href="/facts/Sacred_waters/YYbdWgT6">Sacred waters</a> and <a href="/facts/Flood_myth/2jqChsva">Flood myth</a></p> <p>The importance of rivers throughout <a href="/facts/Human_history/uB3yXt4H">human history</a> has given them an association with <a href="/facts/Life/DNw7NUId">life</a> and <a href="/facts/Fertility/5S7Xull5">fertility</a>. They have also become associated with the reverse, <a href="/facts/Death/VJmq29qm">death</a> and destruction, especially through <a href="/facts/Floods/FDQjJeXW">floods</a>. This power has caused rivers to have a central role in <a href="/facts/Religion/cxntrD0R">religion</a>, <a href="/facts/Ritual/EIJngpmf">ritual</a>, and <a href="/facts/Myth/kG8UTfem">mythology</a>.<a class="footnote-ref" id="fnref:129" href="#fn:129"><sup>129</sup></a> </p><p>In <a href="/facts/Greek_mythology/M7k4FvW8">Greek mythology</a>, the <a href="/facts/Greek_underworld/3JMV6eMT">underworld</a> is bordered by several rivers.<a class="footnote-ref" id="fnref:130" href="#fn:130"><sup>130</sup></a> Ancient Greeks believed that the <a href="/facts/Soul/DJl01SxP">souls</a> of those who perished had to be borne across the <a href="/facts/River_Styx/8gTIvax4">River Styx</a> on a boat by <a href="/facts/Charon/K84MVKrW">Charon</a> in exchange for money.<a class="footnote-ref" id="fnref:131" href="#fn:131"><sup>131</sup></a> Souls that were judged to be good were admitted to <a href="/facts/Elysium/rydSLMID">Elysium</a> and permitted to drink water from the <a href="/facts/Lethe/vXsAzMpT">River Lethe</a> to forget their previous life.<a class="footnote-ref" id="fnref:132" href="#fn:132"><sup>132</sup></a> Rivers also appear in descriptions of <a href="/facts/Paradise/NB9KrK61">paradise</a> in <a href="/facts/Abrahamic_religions/y9z2Wf9q">Abrahamic religions</a>, beginning with the story of <a href="/facts/Genesis_creation_narrative/Fy0E2uD8">Genesis</a>.<a class="footnote-ref" id="fnref:133" href="#fn:133"><sup>133</sup></a> A river beginning in the <a href="/facts/Garden_of_Eden/G52p2uaP">Garden of Eden</a> waters the garden and then splits into four rivers that flow to provide water to the world. These rivers include the <a href="/facts/Tigris%25E2%2580%2593Euphrates_river_system/kg6LGEav">Tigris and Euphrates</a>, and two rivers that are possibly apocryphal but may refer to the <a href="/facts/Nile/vGoXVUFH">Nile</a> and the <a href="/facts/Ganges/q0IGurvB">Ganges</a>.<a class="footnote-ref" id="fnref:134" href="#fn:134"><sup>134</sup></a> The <a href="/facts/Quran/39rkStko">Quran</a> describes these four rivers as flowing with water, milk, wine, and honey, respectively.<a class="footnote-ref" id="fnref:135" href="#fn:135"><sup>135</sup></a> </p><p>The book of Genesis also contains a <a href="/facts/Genesis_flood_narrative/EbjQQLmK">story of a great flood</a>.<a class="footnote-ref" id="fnref:136" href="#fn:136"><sup>136</sup></a> Similar myths are present in the <a href="/facts/Epic_of_Gilgamesh/38VrUaDY">Epic of Gilgamesh</a>, <a href="/facts/Sumer/bxRz093q">Sumerian</a> mythology, and in other cultures.<a class="footnote-ref" id="fnref:137" href="#fn:137"><sup>137</sup></a><a class="footnote-ref" id="fnref:138" href="#fn:138"><sup>138</sup></a> In Genesis, the flood's role was to cleanse Earth of the wrongdoing of humanity. The act of water working to cleanse humans in a ritualistic sense has been compared to the Christian ritual of <a href="/facts/Baptism/wEY6gtGA">baptism</a>, famously the <a href="/facts/Baptism_of_Jesus/8ofnDTjv">Baptism of Jesus</a> in the <a href="/facts/Jordan_River/dRFFQcxV">Jordan River</a>.<a class="footnote-ref" id="fnref:139" href="#fn:139"><sup>139</sup></a> Floods also appear in <a href="/facts/Norse_mythology/hEKfeQql">Norse mythology</a>, where the world is said to emerge from a void that eleven rivers flowed into. <a href="/facts/Aboriginal_Australian/DNAQ5z5m">Aboriginal Australian</a> religion and <a href="/facts/Mesoamerican/cFjUFklr">Mesoamerican</a> mythology also have stories of floods, some of which contain no survivors, unlike the Abrahamic flood.<a class="footnote-ref" id="fnref:140" href="#fn:140"><sup>140</sup></a> </p> <p>Along with mythological rivers, religions have also cared for specific rivers as sacred rivers.<a class="footnote-ref" id="fnref:141" href="#fn:141"><sup>141</sup></a> The <a href="/facts/Ancient_Celtic_religion/FKgV8XEV">Ancient Celtic religion</a> saw rivers as goddesses. The Nile had many gods attached to it. The tears of the goddess <a href="/facts/Isis/agpVzR4K">Isis</a> were said to be the cause of the river's yearly flooding, itself personified by the goddess <a href="/facts/Hapi_(Nile_god)/gS5rmsra">Hapi</a>. Many African religions regard certain rivers as the originator of life. In <a href="/facts/Yoruba_religion/kYeSmLKF">Yoruba religion</a>, <a href="/facts/Yem%25E1%25BB%258Dja/AR2PUWsk">Yemọja</a> rules over the <a href="/facts/Ogun_River/50Q29SX2">Ogun River</a> in modern-day <a href="/facts/Nigeria/gbW17BX8">Nigeria</a> and is responsible for creating all children and fish.<a class="footnote-ref" id="fnref:142" href="#fn:142"><sup>142</sup></a> Some sacred rivers have religious prohibitions attached to them, such as not being allowed to drink from them or ride in a boat along certain stretches. In these religions, such as that of the <a href="/facts/Altai_people/HDACsvdd">Altai</a> in <a href="/facts/Russia/jfkCwyxn">Russia</a>, the river is considered a living being that must be afforded respect.<a class="footnote-ref" id="fnref:143" href="#fn:143"><sup>143</sup></a> </p><p>Rivers are some of the most sacred places in Hinduism.<a class="footnote-ref" id="fnref:144" href="#fn:144"><sup>144</sup></a> There is archeological evidence that mass ritual bathing in rivers at least 5,000 years ago in the <a href="/facts/Indus_River/7vTRHA4t">Indus river valley</a>.<a class="footnote-ref" id="fnref:145" href="#fn:145"><sup>145</sup></a> While most rivers in India are revered, the Ganges is most sacred.<a class="footnote-ref" id="fnref:146" href="#fn:146"><sup>146</sup></a> The river has a central role in various Hindu myths, and its water is said to have properties of healing as well as <a href="/facts/Absolution/SFsreKAc">absolution</a> from sins.<a class="footnote-ref" id="fnref:147" href="#fn:147"><sup>147</sup></a> Hindus believe that when the <a href="/facts/Cremated/2SkhoCly">cremated</a> remains of a person is released into the Ganges, their soul is released from the mortal world.<a class="footnote-ref" id="fnref:148" href="#fn:148"><sup>148</sup></a> </p> <h2 id="threats">Threats</h2> <p><a href="/facts/Freshwater_fish/zqcg3Hmy">Freshwater fish</a> make up 40% of the world's fish species, but 20% of these species are known to have gone extinct in recent years.<a class="footnote-ref" id="fnref:149" href="#fn:149"><sup>149</sup></a> Human uses of rivers make these species especially vulnerable.<a class="footnote-ref" id="fnref:150" href="#fn:150"><sup>150</sup></a> Dams and other engineered changes to rivers can block the migration routes of fish and destroy habitats.<a class="footnote-ref" id="fnref:151" href="#fn:151"><sup>151</sup></a> Rivers that flow freely from headwaters to the sea have better water quality, and also retain their ability to transport nutrient-rich alluvium and other organic material downstream, keeping the ecosystem healthy.<a class="footnote-ref" id="fnref:152" href="#fn:152"><sup>152</sup></a> The creation of a lake changes the habitat of that portion of water, and blocks the transportation of sediment, as well as preventing the natural meandering of the river.<a class="footnote-ref" id="fnref:153" href="#fn:153"><sup>153</sup></a> Dams block the migration of fish such as <a href="/facts/Salmon/7kUsoqVN">salmon</a> for which <a href="/facts/Fish_ladder/76eVn6LK">fish ladder</a> and other bypass systems have been attempted, but these are not always effective.<a class="footnote-ref" id="fnref:154" href="#fn:154"><sup>154</sup></a> </p><p><a href="/facts/Water_pollution/SCUhUYqB">Pollution</a> from factories and urban areas can also damage water quality.<a class="footnote-ref" id="fnref:155" href="#fn:155"><sup>155</sup></a><a class="footnote-ref" id="fnref:156" href="#fn:156"><sup>156</sup></a> "<a href="/facts/Per-_and_polyfluoroalkyl_substances/KcNTVbvS">Per- and polyfluoroalkyl substances</a> (PFAS) is a widely used chemical that breaks down at a slow rate.<a class="footnote-ref" id="fnref:157" href="#fn:157"><sup>157</sup></a> It has been found in the bodies of humans and animals worldwide, as well as in the soil, with potentially negative health effects.<a class="footnote-ref" id="fnref:158" href="#fn:158"><sup>158</sup></a> Research into how to remove it from the environment, and how harmful exposure is, is ongoing.<a class="footnote-ref" id="fnref:159" href="#fn:159"><sup>159</sup></a> <a href="/facts/Fertilizer/ysh3r6NJ">Fertilizer</a> from farms can lead to a proliferation of algae on the surface of rivers and oceans, which prevents <a href="/facts/Oxygen/acyn6o8r">oxygen</a> and light from dissolving into water, making it impossible for underwater life to survive in these so-called <a href="/facts/Dead_zone_(ecology)/TPtDu4c7">dead zones</a>.<a class="footnote-ref" id="fnref:160" href="#fn:160"><sup>160</sup></a> </p><p><a href="/facts/Urban_stream/RxXr2g89">Urban rivers</a> are typically surrounded by impermeable surfaces like stone, <a href="/facts/Asphalt_concrete/TTp7fXA6">asphalt</a>, and concrete.<a class="footnote-ref" id="fnref:161" href="#fn:161"><sup>161</sup></a> Cities often have <a href="/facts/Storm_drains/a7DSuple">storm drains</a> that direct this water to rivers. This can cause flooding risk as large amounts of water are directed into the rivers. Due to these impermeable surfaces, these rivers often have very little alluvium carried in them, causing more erosion once the river exits the impermeable area.<a class="footnote-ref" id="fnref:162" href="#fn:162"><sup>162</sup></a> It has historically been common for <a href="/facts/Sewage/aC5N1kls">sewage</a> to be directed directly to rivers via <a href="/facts/Sewerage/bmbN015l">sewer systems</a> without being treated, along with pollution from industry. This has resulted in a loss of animal and plant life in urban rivers, as well as the spread of <a href="/facts/Waterborne_disease/pxM3dqM4">waterborne diseases</a> such as <a href="/facts/Cholera/rk8JfWEp">cholera</a>.<a class="footnote-ref" id="fnref:163" href="#fn:163"><sup>163</sup></a> In modern times, <a href="/facts/Sewage_treatment/bqLgnLnJ">sewage treatment</a> and controls on pollution from factories have improved the water quality of urban rivers.<a class="footnote-ref" id="fnref:164" href="#fn:164"><sup>164</sup></a> </p> <p><a href="/facts/Climate_change/rEN4BDE7">Climate change</a> can change the flooding cycles and water supply available to rivers.<a class="footnote-ref" id="fnref:165" href="#fn:165"><sup>165</sup></a> Floods can be larger and more destructive than expected, causing damage to the surrounding areas. Floods can also wash unhealthy chemicals and sediment into rivers.<a class="footnote-ref" id="fnref:166" href="#fn:166"><sup>166</sup></a> <a href="/facts/Droughts/LVW0rfuV">Droughts</a> can be deeper and longer, causing rivers to run dangerously low.<a class="footnote-ref" id="fnref:167" href="#fn:167"><sup>167</sup></a> This is in part because of a projected loss of <a href="/facts/Snowpack/fdPyL2qQ">snowpack</a> in mountains, meaning that melting snow can't replenish rivers during warm summer months, leading to lower water levels.<a class="footnote-ref" id="fnref:168" href="#fn:168"><sup>168</sup></a> Lower-level rivers also have warmer temperatures, threatening species like salmon that prefer colder upstream temperatures.<a class="footnote-ref" id="fnref:169" href="#fn:169"><sup>169</sup></a> </p><p>Attempts have been made to regulate the exploitation of rivers to preserve their ecological functions.<a class="footnote-ref" id="fnref:170" href="#fn:170"><sup>170</sup></a> Many <a href="/facts/Wetland/9abbP7CR">wetland</a> areas have become protected from development. Water restrictions can prevent the complete draining of rivers. Limits on the construction of dams, as well as <a href="/facts/Dam_removal/MWIQXkpc">dam removal</a>, can restore the natural habitats of river species.<a class="footnote-ref" id="fnref:171" href="#fn:171"><sup>171</sup></a> Regulators can also ensure regular releases of water from dams to keep animal habitats supplied with water.<a class="footnote-ref" id="fnref:172" href="#fn:172"><sup>172</sup></a> Limits on pollutants like <a href="/facts/Pesticides/Uhf4KnwJ">pesticides</a> can help improve water quality.<a class="footnote-ref" id="fnref:173" href="#fn:173"><sup>173</sup></a> </p> <h2 id="extraterrestrial-rivers">Extraterrestrial rivers</h2> <p>Today, the surface of <a href="/facts/Mars/AQGtVvz0">Mars</a> does not have liquid water. All <a href="/facts/Water_on_Mars/uBNTfa37">water on Mars</a> is part of <a href="/facts/Permafrost/SkFC7LMT">permafrost</a> ice caps, or trace amounts of water vapor in the atmosphere.<a class="footnote-ref" id="fnref:174" href="#fn:174"><sup>174</sup></a> However, there is evidence that rivers flowed on Mars for at least 100,000 years.<a class="footnote-ref" id="fnref:175" href="#fn:175"><sup>175</sup></a> The <a href="/facts/Hellas_Planitia/sX6et9v8">Hellas Planitia</a> is a crater left behind by an impact from an asteroid. It has <a href="/facts/Sedimentary_rock/HQDCjrco">sedimentary rock</a> that was formed 3.7 billion years ago, and <a href="/facts/Lava_field/apwqKYw4">lava fields</a> that are 3.3 billion years old.<a class="footnote-ref" id="fnref:176" href="#fn:176"><sup>176</sup></a> High resolution images of the surface of the plain show evidence of a river network, and even river deltas.<a class="footnote-ref" id="fnref:177" href="#fn:177"><sup>177</sup></a><a class="footnote-ref" id="fnref:178" href="#fn:178"><sup>178</sup></a> These images reveal <a href="/facts/Channel_(geography)/zanMS2Ek">channels</a> formed in the rock, recognized by geologists who study rivers on Earth as being formed by rivers,<a class="footnote-ref" id="fnref:179" href="#fn:179"><sup>179</sup></a> as well as "bench and slope" landforms, outcroppings of rock that show evidence of river erosion. Not only do these formations suggest that rivers once existed, but that they flowed for extensive time periods, and were part of a water cycle that involved precipitation.<a class="footnote-ref" id="fnref:180" href="#fn:180"><sup>180</sup></a> </p><p>The term <a href="/facts/Flumen_(planetary_geology)/nmnWbJX6"><i>flumen</i></a>, in <a href="/facts/Planetary_geology/7C3FXCe9">planetary geology</a>, refers to channels on <a href="/facts/Saturn/D54LcGJ9">Saturn</a>'s moon <a href="/facts/Titan_(moon)/lg0l9PCH">Titan</a> that may carry liquid.<a class="footnote-ref" id="fnref:181" href="#fn:181"><sup>181</sup></a><a class="footnote-ref" id="fnref:182" href="#fn:182"><sup>182</sup></a> Titan's rivers flow with liquid <a href="/facts/Methane/kBHneYnh">methane</a> and <a href="/facts/Ethane/BGCzc6yh">ethane</a>. There are river valleys that exhibit <a href="/facts/Coastal_erosion/nIj8kCHP">wave erosion</a>, seas, and oceans.<a class="footnote-ref" id="fnref:183" href="#fn:183"><sup>183</sup></a> Scientists hope to study these systems to see how coasts erode without the influence of human activity, something that isn't possible when studying terrestrial rivers.<a class="footnote-ref" id="fnref:184" href="#fn:184"><sup>184</sup></a> </p> <h2 id="rivers-by-amount-of-discharge">Rivers by amount of discharge</h2> <p class="note">Main article: <a href="/facts/List_of_rivers_by_discharge/0TEbyyGR">List of rivers by discharge</a></p> <h2 id="see-also">See also</h2> <h3>General</h3> <ul><li><a href="/facts/Lists_of_rivers/xmMdbKkQ">Lists of rivers</a></li> <li><a href="/facts/List_of_waterfalls/10GAB7Bo">List of waterfalls</a></li> <li><a href="/facts/Salt_tide/DsVv2EbQ">Salt tide</a></li> <li><a href="/facts/Water_conflict/7bAf1UpS">Water conflict</a></li> <li><a href="/facts/Freshwater_environmental_quality_parameters/zT1AMQAh">Freshwater environmental quality parameters</a></li> <li><a href="/facts/Potamology/LntaFCBJ">Potamology</a></li> <li><a href="/facts/Limnology/1nHcCAkn">Limnology</a></li> <li><a href="/facts/Morge_(tributary_of_the_Rh%25C3%25B4ne)/ojhdEJrL">Morge (tributary of the Rhône)</a></li></ul> <h3>Crossings</h3> <ul><li><a href="/facts/Bridge/vBJ7Hw8v">Bridge</a></li> <li><a href="/facts/Ferry/5ysqHULA">Ferry</a></li> <li><a href="/facts/Ford_(crossing)/CzohBmw3">Ford</a></li> <li><a href="/facts/Tunnel/PJNSaSIw">Tunnel</a></li></ul> <h3>Transport</h3> <ul><li><a href="/facts/Barge/dmlje4SW">Barge</a></li> <li><a href="/facts/Raft/F3WPhFWK">Raft</a></li> <li><a href="/facts/River_transport/rB1EQAfm">River transport</a></li> <li><a href="/facts/Riverboat/xFM1DwJJ">Riverboat</a></li> <li><a href="/facts/Sailing/QsXNsSLR">Sailing</a></li> <li><a href="/facts/Steamboat/6YpKwFfp">Steamboat</a></li> <li><a href="/facts/Towpath/HTgPjeyM">Towpath</a></li> <li><a href="/facts/Yacht/1H6xRy1U">Yacht</a></li></ul> <h2 id="external-links">External links</h2> <ul><li> Rivers portal</li> <li> Environment portal</li> <li> Ecology portal</li> <li> Rivers at Wikibooks</li></ul> <h2 id="references">References</h2> <ol> <li id="fn:1"><p>"River". Cambridge Dictionary. <a href="https://dictionary.cambridge.org/us/dictionary/english/river" target="_blank">https://dictionary.cambridge.org/us/dictionary/english/river</a> <a href="#fnref:1" class="footnote-back-ref">↩</a></p></li> <li id="fn:2"><p>"River". Cambridge Dictionary. <a href="https://dictionary.cambridge.org/us/dictionary/english/river" target="_blank">https://dictionary.cambridge.org/us/dictionary/english/river</a> <a href="#fnref:2" class="footnote-back-ref">↩</a></p></li> <li id="fn:3"><p>Langbein, W.B.; Iseri, Kathleen T. (1995). "Hydrologic Definitions: Stream". Manual of Hydrology: Part 1. General Surface-Water Techniques (Water Supply Paper 1541-A). Reston, VA: United States Geological Survey. Archived from the original on 9 May 2012. <a href="https://water.usgs.gov/wsc/glossary.html#Stream" target="_blank">https://water.usgs.gov/wsc/glossary.html#Stream</a> <a href="#fnref:3" class="footnote-back-ref">↩</a></p></li> <li id="fn:4"><p>Langbein, W.B.; Iseri, Kathleen T. (1995). "Hydrologic Definitions: Stream". Manual of Hydrology: Part 1. General Surface-Water Techniques (Water Supply Paper 1541-A). Reston, VA: United States Geological Survey. Archived from the original on 9 May 2012. <a href="https://water.usgs.gov/wsc/glossary.html#Stream" target="_blank">https://water.usgs.gov/wsc/glossary.html#Stream</a> <a href="#fnref:4" class="footnote-back-ref">↩</a></p></li> <li id="fn:5"><p>Langbein, W.B.; Iseri, Kathleen T. (1995). "Hydrologic Definitions: Stream". Manual of Hydrology: Part 1. General Surface-Water Techniques (Water Supply Paper 1541-A). Reston, VA: United States Geological Survey. Archived from the original on 9 May 2012. <a href="https://water.usgs.gov/wsc/glossary.html#Stream" target="_blank">https://water.usgs.gov/wsc/glossary.html#Stream</a> <a href="#fnref:5" class="footnote-back-ref">↩</a></p></li> <li id="fn:6"><p>"Rivers, Streams, and Creeks | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks</a> <a href="#fnref:6" class="footnote-back-ref">↩</a></p></li> <li id="fn:7"><p>"Rivers, Streams, and Creeks | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks</a> <a href="#fnref:7" class="footnote-back-ref">↩</a></p></li> <li id="fn:8"><p>"Rivers and the Landscape | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-and-landscape" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-and-landscape</a> <a href="#fnref:8" class="footnote-back-ref">↩</a></p></li> <li id="fn:9"><p>"Rivers and the Landscape | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-and-landscape" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-and-landscape</a> <a href="#fnref:9" class="footnote-back-ref">↩</a></p></li> <li id="fn:10"><p>"River Systems and Fluvial Landforms – Geology (U.S. National Park Service)". National Park Service. Retrieved 14 July 2024. <a href="https://www.nps.gov/subjects/geology/fluvial-landforms.htm" target="_blank">https://www.nps.gov/subjects/geology/fluvial-landforms.htm</a> <a href="#fnref:10" class="footnote-back-ref">↩</a></p></li> <li id="fn:11"><p>"Rivers and the Landscape | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-and-landscape" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-and-landscape</a> <a href="#fnref:11" class="footnote-back-ref">↩</a></p></li> <li id="fn:12"><p>"Rivers and the Landscape | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-and-landscape" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-and-landscape</a> <a href="#fnref:12" class="footnote-back-ref">↩</a></p></li> <li id="fn:13"><p>"Rivers and the Landscape | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-and-landscape" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-and-landscape</a> <a href="#fnref:13" class="footnote-back-ref">↩</a></p></li> <li id="fn:14"><p>"Rivers, Streams, and Creeks | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks</a> <a href="#fnref:14" class="footnote-back-ref">↩</a></p></li> <li id="fn:15"><p>"Rivers, Streams, and Creeks | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks</a> <a href="#fnref:15" class="footnote-back-ref">↩</a></p></li> <li id="fn:16"><p>"Rivers, Streams, and Creeks | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks</a> <a href="#fnref:16" class="footnote-back-ref">↩</a></p></li> <li id="fn:17"><p>"Rivers, Streams, and Creeks | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks</a> <a href="#fnref:17" class="footnote-back-ref">↩</a></p></li> <li id="fn:18"><p>"Rivers, Streams, and Creeks | U.S. Geological Survey". United States Geological Survey. 6 June 2018. Retrieved 14 July 2024. <a href="https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks" target="_blank">https://www.usgs.gov/special-topics/water-science-school/science/rivers-streams-and-creeks</a> <a href="#fnref:18" class="footnote-back-ref">↩</a></p></li> <li id="fn:19"><p>Warner, Hugh (2 July 2024). "What determines the directional flow of rivers in the United States?". Geographic FAQ Hub: Answers to Your Global Questions. Retrieved 1 August 2024. <a href="https://www.ncesc.com/geographic-faq/what-determines-the-directional-flow-of-rivers-in-the-united-states/" target="_blank">https://www.ncesc.com/geographic-faq/what-determines-the-directional-flow-of-rivers-in-the-united-states/</a> <a href="#fnref:19" class="footnote-back-ref">↩</a></p></li> <li id="fn:20"><p>Warner, Hugh (2 July 2024). "What determines the directional flow of rivers in the United States?". Geographic FAQ Hub: Answers to Your Global Questions. Retrieved 1 August 2024. <a href="https://www.ncesc.com/geographic-faq/what-determines-the-directional-flow-of-rivers-in-the-united-states/" target="_blank">https://www.ncesc.com/geographic-faq/what-determines-the-directional-flow-of-rivers-in-the-united-states/</a> <a href="#fnref:20" class="footnote-back-ref">↩</a></p></li> <li id="fn:21"><p>"Rivers and the Landscape | U.S. Geological Survey". United States Geological Survey. 6 June 2018. 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