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Side valley

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Side valleys and tributary valleys are valleys whose brooks or riversflow into greater ones. Upstream, the valleys can be classified in an increasing order which is equivalent to the usual orographic order: the tributaries are ordered from those nearest to the source of the river to those nearest to the mouth of the river. A confluence is where two or more tributaries or rivers flow together. Orographic order (e.g.

River Ouse, YorkshireRiver Ouse, YorkshireThe River Ouse ( ) is a river in North Yorkshire, England. Hydrologically, the river is a continuation of the River Ure, and the combined length of the River Ure and River Ouse makes it, at 129 miles (208 km), the sixth-longest river of the United Kingdom and (including the Ure) the longest to flow entirely in one county. The length of the Ouse alone is about 52 miles (84 km) but the total length of the river is disputed.ValleyValleyA valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas.TributaryTributaryA tributary, or an affluent, is a stream that typically flows into a larger stream (main stem or parent) or lake, or rarely into a smaller stream, e.g., the Esla tributary to the Douro. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem into which they flow drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean, another stream, or into an endorheic basin.River ThamesRiver ThamesRiver in southern England 0Thames Head1A433 Fosse Way/Tetbury Road Thames Bridge 2bridleway bridge 3A429 Bridge 4Parker's Bridge for Thames Path ("TP") 5unnamed (the south) lane, Ewen (to/from Poole Keynes) & for TP 6Former Washburn's Mill footbridge for TP 7footbridge above Old Mill Farm 8footbridge 9footbridge above Neigh Bridge Lake for TP 10Neigh Bridge 11Oaksey Road Bridge for TP 11Cul de sac bridge Cotswold Water Park hamlet 12Lower Mill Estate bridge 1 13Lower Mill Es…OceanOceanBody of salt water covering most of EarthThe ocean is the body of salt water that covers approximately 70.8% of Earth. The ocean is conventionally divided into large bodies of water, which are also referred to as oceans (in descending order by area: the Pacific Ocean, the Atlantic Ocean, the Indian Ocean, the Antarctic/Southern Ocean, and the Arctic Ocean), and are themselves mostly divided into seas, gulfs and subsequent bodies of water.HumberHumberThe Humber is a large tidal estuary on the east coast of Northern England. It is formed at Trent Falls, Faxfleet, by the confluence of the tidal riversOuse and Trent. From there to the North Sea, it forms part of the boundary between the East Riding of Yorkshire on the north bank and North Lincolnshire on the south bank. Also known as the River Humber, it is tidal its entire length.RiverRiverA river is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth.River sourceRiver sourceThe source or headwater of a river or stream is the geographical point of its beginning, specifically where surface runoff water begins to accumulate into a flowing channel of water. A river or stream into which one or many tributary rivers or streams flow has many headwaters, these being all of the individual headwaters of its tributaries.River deltaRiver deltaA river delta is a landform, typically triangular, created by the deposition of the sediments that are carried by the waters of a river, where the river merges with a body of slow-moving water or with a body of stagnant water. The creation of a river delta occurs at the river mouth, where the river merges into an ocean, a sea, or an estuary, into a lake, a reservoir, or (more rarely) into another river that cannot carry away the sediment supplied by the feeding river.StreamStreamA stream is a continuous body of surface water flowing within the bed and banks of a channel. The channel is a watercourse, although the watercourse may be seasonally or periodically dry. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. A long, large stream is usually called a river, while a smaller, less voluminous, and more intermittent stream is known as a creek or tributary, among other names.ConfluenceConfluenceIn geography, a confluence (also conflux) occurs where two or more watercourses join to form a single channel.OrographyOrographyOrography is the study of the topographic relief of mountains, and can more broadly include hills, water stream directions and any part of a region's elevated terrain. Orography (also known as oreography, orology, or oreology) falls within the broader discipline of geomorphology. The term orography comes from the Greek: όρος, hill, γράφω, to write.

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