A well-defined network of channels that exhibit typical stream features, such as meanders, riffles, and pools, indicates a landscape shaped by streams. Additionally, the presence of floodplains and alluvial fans in the area may suggest stream activity has played a significant role in shaping the landscape.
Mountain streams are typically in the youthful stage of development. These streams have steep gradients, fast flows, and are actively eroding the surrounding landscape. They are characterized by high energy and are often creating V-shaped valleys.
Glaciers can form various landscape features, including U-shaped valleys, cirques, aretes, and moraines. These features are created as glaciers erode and deposit material as they flow over the land.
Wide streams and valleys typically have a large water flow capacity, which can accommodate high volumes of water. They often have gently sloping sides and bottoms, creating a broad and open landscape. Wide streams and valleys can also support a diverse range of plant and animal species due to the availability of space and resources.
Boreal forests, also known as taiga forests, are found in northern Europe, Asia, and North America where cold lakes and streams are part of the landscape. These forests are characterized by coniferous trees, such as spruce, fir, and pine, and have adapted to cold and harsh conditions. They are an important habitat for various wildlife species like bears, wolves, and moose.
V-shaped valleys are commonly found in mountainous regions where rivers or streams have eroded the land over time. They are formed through the process of downcutting, where water gradually wears away the rock and sediment, creating a distinctive V shape in the landscape.
In a youthful stage of valley evolution, downcutting streams erode the land vertically, carving deeper channels and creating steep-walled valleys. These streams have high energy and are actively eroding the landscape, leading to the formation of V-shaped valleys characteristic of early stages of valley development.
they lived by rivers and streams
They erode the landscaping around them.
Eskers are formed by meltwater streams flowing within or beneath glaciers during the last Ice Age. As the glaciers melted, the sediment and rocks carried by the streams were deposited in long, winding ridges. The unique formation of eskers is primarily due to the deposition of sediment by these meltwater streams, as well as the reshaping of the landscape by the movement of the glaciers.
Sedimentation can lead to the deposition of sediments on stream beds, impacting water flow, aquatic habitats, and channel morphology. Erosion can result in the removal of sediment from stream banks and beds, causing channel widening, habitat disruption, and potential downstream sediment delivery.
On an Ordnance Survey map, a waterfall is represented by a blue triangle pointing downward. This symbol indicates the location of the waterfall within the landscape. Additionally, the surrounding water features may also be marked with blue lines to represent rivers or streams.
Mountain streams are typically in the youthful stage of development. These streams have steep gradients, fast flows, and are actively eroding the surrounding landscape. They are characterized by high energy and are often creating V-shaped valleys.
Salmon primarily live in saltwater environments, such as oceans and seas, but they migrate to freshwater rivers and streams to spawn.
Karst landscape is characterized by soluble rocks such as limestone, dolomite, and gypsum that are eroded by water to produce unique features like sinkholes, caves, and underground drainage systems. This type of landscape is known for its distinctive topography and the presence of disappearing streams and underground rivers.
The collective noun for a stream is often referred to as a "network" or "system" of streams. In some contexts, you might also hear "flow" or "course" used to describe multiple streams. These terms emphasize the interconnectedness and movement of water in a landscape.
In landlocked lakes, water is primarily discharged through evaporation, groundwater seepage, and rivers and streams that flow into or out of the lake. Precipitation also contributes to the water balance of a lake by adding water to the system.
Canyons are primarily formed by water erosion, typically from rivers or streams. The flowing water cuts through the rock over time, shaping the landscape into deep, narrow valleys. Additionally, other factors such as glaciers, wind, and tectonic activities can contribute to the erosion and formation of canyons.