I Can’t Sleep - Streams | Gentle Bedtime Reading for Sleep

Episode Date: November 5, 2024

Ease into sleep with this calm bedtime reading about streams, the small flowing waterways that shape landscapes and nourish life. As you listen, Benjamin’s soothing narration will guide you through the natural beauty, formation, and importance of streams in the environment. With a peaceful cadence, he shares fact-filled storytelling—no whispers, no hypnosis—just calm, educational reading to ease insomnia and quiet restless thoughts. Perfect for reducing stress and helping you drift into restful sleep. Press play, relax, and let your mind follow the gentle flow of streams. Want More? Request a Topic: https://www.icantsleeppodcast.com/request-a-topic Ad-Free Episodes: https://icantsleep.supportingcast.fm/ Shop Sleep-Friendly Products: https://www.icantsleeppodcast.com/sponsors Join the Discussion on Discord: https://discord.gg/myhGhVUhn7 This content is derived from the Wikipedia article on Streams, available under the Creative Commons Attribution-ShareAlike (CC BY-SA) license. Read the full article: Wikipedia – Streams. Happy sleeping! Learn more about your ad choices. Visit megaphone.fm/adchoices

You're listening to a Glassbox media podcast. What if I told you that most of the modern day self-help advice you've been hearing could actually make you worse? The key to a better life isn't about feel-good gimmicks that sound catchy. The Mentally Stronger Podcast gives you access to a licensed therapist who shares science-backed tools that will actually change your life. Hi, I'm Amy Morin, psychotherapist, mental strength trainer, and international best-selling author. In each episode, we cover research-back strategies, like how to stop relying on willpower and start creating habits for lasting change. And the five mental strength-building exercises you can do from your couch.

I also speak to world-class experts like Dr. Nicole Kane, who shares how to permanently heal anxiety by addressing the root cause. With over 200 episodes in our catalog, this podcast is for you if you're ready to crush self-doubt, conquer challenges, and become stronger than ever with therapist-approved strategies that can change your life. Listen to Mentally Stronger with Therapist Amy Morin, wherever you get your podcasts. Welcome to the I Can't Sleep podcast, where I read random articles from across the web to bore you to sleep with my soothing voice. I'm your host, Benjamin Boster. Today's episode is from a Wikipedia article titled, Stream. Before we

get started, I want to thank everyone who submitted topics. Your support has been incredible, and we've received hundreds of suggestions. If you'd like to hear your topic sooner, I now offer three options to bump your topic to the top of the list. Just visit I Can't Sleep Podcast.com and click on the request to topic link in the navigation. Each option has a small cost, and it's a great way to hear exactly what you want next, while supporting the show. Now let's get onto today's episode. A stream is a continuous body of surface water flowing within the bed and banks of a channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names.

Long, large streams are usually called rivers, while smaller, less voluminous and more intermittent streams are known as stream. streamlets, brooks, or creeks. The flow of a stream is controlled by three inputs, surface runoff from precipitation or meltwater, daylighted subterranean water, and surface groundwater, spring water. The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled. more by long-term patterns of precipitation. The stream encompasses surface, subsurface, and groundwater fluxes that respond to geological, geomorphological, hydrological, and biotic controls.

Streams are important as conduits in the water cycle, instruments in groundwater recharge, and corridors for fish and wildlife migration. The biological habitat in the immediate vicinity of a stream is called a riparian zone. Given the status of the ongoing Holocene extinction, streams play an important core or role in connecting fragmented habitats and thus in conserving biodiversity. A study of streams and waterways in general is known as surface hydrology and is a core element of environmental geography.

A brook is a stream smaller than a creek, especially one that is fed by a spring or seep. It is usually small and easily forded. A brook is characterized by its shallowness. Another is a creek or creek. In Australia, Canada, New Zealand, and the United States, a narrow stream that is smaller than a river, a minor tributary of a river, a brook.

Sometimes navigable by watercraft and may be intermittent. In the United Kingdom, India, and parts of Maryland, New England, a tidal inlet, typically in a salt marsh or mangrove swamp, or between enclosed and drained former salt marshes or swamps, e.g. Portsbridge Creek, separating Portsea Island from the mainland. In these cases, the stream is the tidal stream, the course of the seawater through the creek channel at low and high tide.

In hydrography, gut is a small creek. This is seen in proper names in eastern North America from the mid-Atlantic states. For instance, the gut in Pennsylvania, ash gut and Delaware, and other streams, down into the Caribbean. For instance, guinea gut, fish bay gut, cob gut, battery gut. gut and other rivers and streams in the United States Virgin Islands in Jamaica, Sandy Gut, Ben's Gut River, White Gut River, and in many streams and creeks of the Dutch Caribbean. A river is a large natural stream that is much wider and deeper than a creek, and not easily fordable and may be a navigable waterway. The linear channel between the parallel ridges

or bars on a shoreline beach or river floodplain, or between a bar on the shore is called a runnal. It's also called a swale. A tributary is a contributory stream to a larger stream, or a stream which does not reach a static body of water such as a lake, bay, or ocean, but joins another river, a parent river. Sometimes this is also called a branch or fork. A distributory, A distributory or distributory channel is a stream that branches off and flows away from a mainstream channel, and the phenomenon is known as river bifurcation. Distributaries are common features of river deltas, and are often found where a valley stream enters wide flatlands,

or approaches the coastal plains around a lake or an ocean. They can also occur inland on alluvial fans or where tributary stream bifurcades as it nears its confluence with a larger stream. Common terms for individual river distributaries in English-speaking countries are arm and channel. There are a number of regional names for a stream. In North America, the following.

Branch is used to name streams in Maryland and Virginia. Creek is common throughout the United States, as well as Australia. Falls is also used to name streams in Maryland for streams or rivers which have waterfalls on them, even if such falls only have a small vertical drop. Little Gunpowder Falls and Jones Falls are actually rivers named in this manner, unique to Maryland. Kill in New York, Pennsylvania, Delaware, and New Jersey comes from a Dutch language word meaning riverbed or water channel and can also be used for the UK meaning of Creek. Run in Ohio, Maryland, Michigan, New Jersey, Pennsylvania, Virginia, or West Virginia can be the name

of a stream. Run in Florida is the name given to streams coming out of small, natural springs. River is used for streams from larger springs like the Silver River and Rainbow River. Stream and Brook are used in Midwestern states, Mid-Atlantic states, and New England. In the United Kingdom, Alt is used in the Scottish Highlands. Beck is used in areas between Lincolnshire and Cumbria and areas which were once occupied by the Danes and Norwegians. Born or Winterbourne is used in the chalk downland of southern England for ephemeral rivers. When permanent, they are chalk streams. Bern is used in Scotland and northeast England.

Gill is seen in the north of England and Kent and Surrey influenced by Old Norse. The variant Gill, spelled G-H-Y-L-L, is used in the Lake District and appears to have been an invention of William Wordsworth. Nant is used in Wales. Rivulet is a term encountered in Victorian-era publications. Scyc is used in the Scottish lowlands in Cumbria for a seasonal stream. Some related terminology. Bar.

A shoal that develops in a stream as sediment is deposited as the current slows or is impeded by wave action at the confluence. bifurcation A fork into two or more streams Channel A depression created by constant erosion That carries the streams flow Confluence

The point at which the two streams merge If the two tributaries are of approximately equal size The confluence may be called a fork Drainage Basin Also known as a water-short in the United States. The area of land where water flows into a stream. A large drainage basin such as the Amazon River contains many smaller drainage basins.

Floodplain. Lands adjacent to the stream that are subject to flooding when a stream overflows its banks. Headwaters or source. The part of a stream or river proximate to its source. The word is most commonly used in the plural where there is no single point source. Nick Point The point on a stream's profile where a sudden change in the stream gradient occurs. Mouth

The point at which the stream discharges, possibly via an estuary or delta, into a static body of water such as a lake or ocean, pool, a segment where the water is deeper and slower moving. Rapids, a turbulent fast-flowing stretch of a stream or river. Riffel A segment where the flow is shallower and more turbulent. River, a large natural stream which may be a waterway. Run, a somewhat smoothly flowing segment of the stream, spring.

the point at which a stream emerges from an underground course through unconsolidated sediments or through caves. A stream can, especially with caves, flow above ground for part of its course and underground for part of its course. Stream bed. The bottom of a stream. Stream corridor. Stream, its floodplains, and the transitional upland fringe. stream flow the water moving through a stream channel stream gauge a side along the route of a stream river used for reference marking or water monitoring tallweg the river's longitudinal section or the line joining the deepest point in the channel at each stage from source to mouth water course a channel followed by a stream, a flowing body of water, or the stream itself.

In the UK, some aspects of criminal law, such as the Rivers Prevention of Pollution Act 1951, specify that a water course includes those rivers which are dry for part of the year. In some jurisdictions, owners of land over which the water flows may have the legal right to use or retain some or much of that water. This right may extend to estuaries, rivers, streams, anabranches, and canals, waterfall or cascade. The fall of water where this stream goes over a sudden drop called a nickpoint. Some nickpoints are formed by erosion when water flows over

and especially resistant stratum, followed by one less so. The stream expends kinetic energy in trying to eliminate the nickpoint, wetted perimeter, the line on which the stream surface meets the channel walls. A stream source depends on the surrounding landscape and its function within larger river networks. While perennial and intermittent streams are typically supplied by smaller upstream waters and groundwater, headwater and ephemeral streams often derive most of their water from precipitation in the form of rain and snow. Most of this precipitated water re-enters the atmosphere by evaporation from soil and water bodies, or by the evapotranspiration of plants.

Some of the water proceeds to sink into the earth by infiltration and becomes groundwater, much of which eventually enters streams. Some precipitated water is temporarily locked up in snowfields and glaciers, to be released later by evaporation or melting. The rest of the water flows off the land as runoff, the proportion of which varies according to many factors, such as wind, humidity, vegetation, rock types, and relief. This runoff starts as a thin film called sheetwash,

combined with a network of tiny rills, together constituting sheet runoff. When this water is concentrated in a channel, a stream has its birth. Some creeks may start from ponds or lakes. Fresh waters, primary sources, or precipitation in mountain snow melt. However, rivers typically originate in the highlands and are slowly created by the erosion of mountain snowmelt into lakes or rivers. Rivers usually flow from their source topographically and erode as they pass until they reach the base stage of erosion. Scientists have offered a way based on data to define the origin of the lake. A classified sample was the one measured by the Chinese researchers from

the University of Chinese Academy of Sciences. The source of a river or stream, its point of origin, can consist of lakes, swamps, springs, or glaciers. A typical river has several tributaries. Each of these may be made up of several other smaller tributaries, so that together this stream and all its tributaries are called a drainage network. Although each tributary has its own source, international practice is to take the source farthest from the river mouth as the source of the entire river system.

from which the most extended length of the river measured as a starting point is taken as the length of the whole river system and that furthest starting point is conventionally taken as the source of the whole river system. For example, the origin of the Nile River is the confluence of the white Nile and the Blue Nile, but the source of the whole river system is in its upper reaches. If there is no specific designation, length of the Nile refers to the river length of the Nile system, rather than to the length of the Nile River from the point where it's formed by a confluence of tributaries. The Nile's source is often cited as Lake Victoria, but the lake has significant feeder rivers. The Kigera River, which flows into Lake Victoria near Bukoba's Tanzanian-Tam.

town is the longest feeder, though sources do not agree on which is the Kigura's longest tributary, and therefore the Nile's most remote source itself. To qualify as a stream, a body of water must be either recurring or perennial. Recurring, intermittent streams, have water in the channel for at least part of the year. A stream of the first order is a stream which does not have any other recurrenton. or perennial stream feeding into it. When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream.

Streams of lower order joining a higher-order stream do not change the order of the higher stream. A gradient of a stream is a critical factor in determining its character and is entirely determined by its base level of erosion. The base level of erosion is the point at which the stream either enters the ocean, a lake, or pond, or enters a stretch in which it has a much lower gradient, and may be specifically applied to any particular stretch of a stream. In geological terms, the stream will erode down through its bed to achieve the base level of erosion throughout its course.

If this base level is low, then the stream will rapidly cut through underlying strata and have a steep gradient. And if the base level is relatively high, then the stream will form a floodplain and meander. Typically, streams are said to have a particular elevation profile, beginning with steep gradients, no floodplain, and little shifting of channels, eventually evolving. to streams with low gradients, wide floodplains, and extensive meanders. The initial stage is sometimes termed a young or immature stream, and the later state a mature or old stream. Meanders are looping changes of direction of a stream caused by the erosion and deposition of bank materials. These are typically serpentine and form. Typically, over time, the meanders gradually migrate downstream.

If some resistant material slows or stops the downstream movement of a meander, a stream may erode through the neck between two legs of a meander to become temporarily straighter, leaving behind an arc-shaped body of water termed an oxbow lake or bayou. A flood may also cause a meander to be cut through in this way. The stream load is defined as the solid matter carried by a stream. Streams can carry sediment or alluvium. The amount of load it can carry capacity, as well as the largest object it can carry, competence,

are both dependent on the velocity of the stream. A perennial stream is one which flows continuously all year. Some perennial streams may only have continuous flow and segments, of its stream bed year-round during years of normal rainfall. Blue-line streams are perennial streams and are marked on topographic maps with a solid blue line. The word perennial from the 1640s, meaning evergreen, is established in Latin perennas,

keeping the meaning as everlasting all year-round, her over plus anus year this has been proved since the 1670s by the living years in the sense of bodni the metaphorical sense of enduring eternal originates from 1750 they are related to perennial perennial streams have one or more of these characteristics one direct observation or compelling evidence suggests that there is no interruption in the flow at ground. 2. The existence of one or more specific features of the perennial streams, including riverbed forms, for example, ripples, pools, runs, gravel bars, other depositional characteristics, bed armor, layer, riverbank erosion and or

Polishment. Indications of waterborne debris and sediment transport. Defined river or streambed and banks. 3. The catchment area exceeds 0.25 square miles. 4. USGS regression on the VHT data layer oriented application on the probability of intermittent flow. 5. The existence of a aquatic organisms that require uninterrupted circulation. 6. As shown by bank leakage, spring, or other indicators, grassroots flow mainly supports groundwater recharge. 7. There are high channels of permeability, especially stratospheric, boundary conditions.

While stratospheric groundwater also decreases on occasion. 8. Existence of native aquatic organisms which require undisturbed survival flow. 9. A surrounding topography exhibits features of being formed by fluvial processes. Absence of such characteristics supports classifying a stream as intermittent, showing interruptions in time or space. Generally, streams that flow only during and immediately after precipitate, are termed ephemeral. There is no clear demarcation between surface runoff and an ephemeral stream,

and some ephemeral streams can be classed as intermittent, flow all but disappearing in the normal course of seasons, but ample flow backups, restoring stream presence. Such circumstances are documented when stream beds have opened up a path into mines or other underground chambers. According to official U.S. definitions, the channels of intermittent streams are well-defined, as opposed to ephemeral streams,

which may or may not have a defined channel and rely mainly on storm runoff, as their aquatic bed is above the water table. An ephemeral stream does not have the biological, hydrological and physical characteristics of a continuous or intermittent stream. The same non-perennial channel might change characteristics from intermittent to ephemeral over its course. Washes can fill up quickly during rains, and there may be a sudden torrent of water after a thunderstorm begins upstream, such as during monsoonal conditions.

In the United States, an intermittent or seasonal stream is one that only flows for part of a year and is marked on topographic maps with a line of blue dashes and dots. A wash, desert wash, or Oroyo is normally a dry stream bed in the deserts of the American southwest, which flows after sufficient rainfall. In Italy, an intermittent stream is turned. termed a torrent, Italian torrente. In full flood, the stream may or may not be torrential, in the dramatic sense of the word, but there will be one or more seasons in which the flow is reduced to a trickle or less. Typically torrents have apennin rather than alpine sources,

and in the summer they are fed by little precipitation and no melting snow. In this case, the maximum discharge will be during the spring and autumn. An intermittent stream can also be called a winterborn in Britain, Awadi and Arabic-speaking world, or Torrente or Rambla, this last one from Arabic origin in Spain and Latin America. In Australia, an intermittent stream is usually called a creek and marked on topographic maps with a solid blue line. There are five generic classifications.

Consequent streams are streams whose course is a direct consequence of the original slope of the surface upon which it developed, i.e. streams that follow slope of the land over which they originally formed. Subsequent streams are streams whose course has been determined by selective headward erosion along weak strata. These streams have generally developed after the original stream. Subsequent streams developed independently of the original relief of the land, and generally follow paths determined by the weak rock belts. Ressequent streams are streams whose course follows the original relief,

but at a lower levels than the original slope, e.g. flows down a course determined by the underlying strata in the same direction. These streams develop later and are generally attributory to a subsequent stream. Obsequent streams are streams flowing in the opposite, the direction of the consequent drainage. Insequent streams have an almost random drainage, often forming dendritic patterns. These are typically tributaries, and have developed by a headward erosion on a horizontally stratified belt, or on homogeneous rocks. These streams follow courses that apparently were not controlled by the original slope of the surface, its structure, or the the type of rock. According to the water underneath. Gaining, a stream or path to receive water from

groundwater. Losing. A stream or reach of a stream which shows a net loss of water to groundwater or evaporation. Isolated. The water flow or channel shall not supply or remove water from the saturated region. Purched. Refers to the loss or isolation flow separated from the groundwater in the air zone.