Valley in the context of "Drainage divide"

⭐ In the context of drainage divides, a valley floor divide is most likely formed by what geological processes?

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👉 Valley in the context of Drainage divide

A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern.

A triple divide is a point, often a summit, where three drainage basins meet. A valley floor divide is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides.

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Valley in the context of Evrotas Valley

The Evrotas Valley is an 82 km elongated valley between Taygetus and Parnon which traverses Laconia, Greece. Homer called the valley Kili Lakedemon, while Sparta, Mystras and Gytheio are the main cities within the valley. It is one of the largest valleys in Greece. The valley is predominantly an agricultural region that contains many citrus groves, olive groves, and pasture lands. It is the location of the largest orange production in the Peloponnese and probably in all of Greece. Lakonia, a brand of orange juice, is based in Amykles. The Evrotas Valley records the highest summer mean maximum temperatures in Greece.

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Valley in the context of Plain

In geography, a plain, commonly known as flatland, is a flat expanse of land that generally has few rapid or steep changes in elevation. Natural vegetation in plains can include prairies/grasslands, forests, savanah, tundra, and desert biomes, among others. Plains occur as lowlands along valleys or at the base of mountains, as coastal plains, and as plateaus or uplands. Plains are one of the major landforms on earth, being present on all continents and covering more than one-third of the world's land area. Plains in many areas are important for agriculture. There are various types of plains, and biomes on them.

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Valley in the context of Pajuniemi

Pajuniemi is a village located in Suodenniemi, Sastamala in Pirkanmaa, Finland. In the east it borders Lake Kourajärvi, in the north the village of Suodenniemi and in the west the border of Pori. In the south, Pajuniemi's neighbors are the villages of Kiikoistenmaa and Kouraniemi. The village itself is located on the edges of the valley opening to Lake Kourajärvi and in the surroundings.

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Valley in the context of Canal

Canals or artificial waterways are waterways or engineered channels built for drainage management (e.g. flood control and irrigation) or for conveyancing water transport vehicles (e.g. water taxi). They carry free, calm surface flow under atmospheric pressure, and can be thought of as artificial rivers.

In most cases, a canal has a series of dams and locks that create reservoirs of low speed current flow. These reservoirs are referred to as slack water levels, often just called levels. A canal can be called a navigation canal when it parallels a natural river and shares part of the latter's discharges and drainage basin, and leverages its resources by building dams and locks to increase and lengthen its stretches of slack water levels while staying in its valley.

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Valley in the context of Landform

A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great oceanic basins.

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Valley in the context of Mountain range

A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets.

Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types.

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Valley in the context of Drin Valley

The Drin Valley (Albanian: Lugina e Drinit) is a valley in northern and eastern Albania along the Drin River.

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Valley in the context of Andros

Andros (Greek: Άνδρος, pronounced [ˈanðros]) is the northernmost island of the Greek Cyclades archipelago, about 10 km (6 mi) southeast of Euboea, and about 3 km (2 mi) north of Tinos. It is nearly 40 km (25 mi) long, and its greatest breadth is 16 km (10 mi). It is for the most part mountainous, with many fruitful and well-watered valleys. The municipality, which includes the island Andros and several small, uninhabited islands, has an area of 380 km (147 sq mi). The largest towns are Andros, Gavrio, Batsi, and Ormos Korthiou.

Palaeopolis, the ancient capital, was built into a steep hillside, and the breakwater of its harbor can still be seen underwater. At the village of Apoikia, there is the notable spring of Sariza, where the water flows from a sculpted stone lion's head. Andros also offers hiking options with many new paths being added each year.

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Valley in the context of Fjord

In physical geography, a fjord (also spelled fiord in New Zealand English; /ˈfjɔːrd, fˈɔːrd/ ) is a long, narrow sea inlet with steep sides or cliffs in a valley created by a former glacier, which has since become inundated with water. They are the glacial equivalent of rias, or drowned river valleys. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. Areas with extensive fjords demonstrate an extreme example of the coastline paradox; Norway's coastline is estimated to be 29,000 km (18,000 mi) long with its nearly 1,200 fjords, but only 2,500 km (1,600 mi) long when excluding the fjords.

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