The Indus Valley Civilization emerged around 2600 BCE in present-day Pakistan and northwest India. It was characterized by advanced city planning, sophisticated drainage systems, and trade networks. The civilization declined around 1900 BCE possibly due to environmental factors, invasions, or economic changes.

The Cotton Valley Branch in Cotton Valley is located in Webster Parish, Louisiana, in the United States. It is a historic railway line that was originally part of the Louisiana and Northwest Railroad before being acquired by Kansas City Southern Railway.

The Valley Springs Branch in Valley Springs is located in Calaveras County, California. It runs through the town of Valley Springs and is part of the Sierra Northern Railway system.

The Valley - H. Grady Bradshaw Chambers County Library is located at 300 Columbus Road, Valley, Alabama, 36854.

The Valley Historical Society in Valley, Washington is located on Main Street in the town of Valley.

The Valley Community Historical Society Inc in Valley, Nebraska, is located at 245 E Reichmuth Road.

The Spring Valley Historical Society in Spring Valley, Minnesota, is located at 201 South Broadway Avenue.

Jiuzhaigou Valley was created by the geological movement of the Earth's crust around 2-3 million years ago. The valley's distinctive landscape features, including its deep gorges, colorful lakes, and waterfalls, are the result of glacial erosion and tectonic activity over time.

Compostela Valley in the Philippines has a total area of approximately 4,668 square kilometers.

"Mountain High... Valley Low," an album by gospel artist Yolanda Adams, was released on September 21, 1999. It includes songs like "Open My Heart" and "I Believe I Can Fly."

A valley between ridges is a low-lying area typically enclosed by higher elevation on both sides. It is formed through various geological processes such as erosion by rivers and glaciers or tectonic activity. Valleys between ridges often provide passage for water flow or access between two areas.

the water is getting to high elevations

Valleys with a U-shape are typically carved by glaciers, which erode the valley floor and walls more uniformly. Valleys with a V-shape are usually formed by rivers through the process of water erosion, which carves a more narrow and steep valley.

To draw a rift valley, start by drawing two parallel lines to represent the edges of the valley. Then, add lines or shading to indicate the downward slope from the edges towards the center. You can also include details like mountain ranges or rivers that are often found along rift valleys.

A fjord is a coastal valley that has been carved out by glacial action.

Ridges and valleys are geological landforms characterized by their alternating patterns of elevated areas (ridges) and lower areas (valleys). They are typically formed by tectonic forces, erosion, and other natural processes. In some cases, human activities such as mining and agriculture can also influence the formation of ridges and valleys.

Some prominent features of a narrow V-shaped valley with a stream profile that drops rapidly include steep, rocky walls, minimal vegetation due to the harsh environment, a high-gradient stream flowing through the valley, and the potential for waterfalls and cascades as the stream descends quickly.

Living in a V-shaped valley can be dangerous due to the risk of flash floods and rockfalls, as water and debris can funnel down the narrow valley, causing rapid and unpredictable flooding. The steep slopes of the valley can also increase the potential for landslides and rockslides, posing a threat to residents living below.

It is formed by an upwelling of hot mantle material under the valley (which has elevated the land) and then split it as the hot mantle moves sideways away form the center of upwelling. This results in volcanoes and a Graben fault system (a rift valley) above the upwelling. Essentially the Rift Valley is the start of a new ocean - the two sides of Africa are splitting apart.

Both valleys and plains are low-lying areas of land. Valleys are typically formed by the erosion of river or glacial activity, while plains are generally flat expanses of land with minimal elevation changes. Both landforms can be rich in fertile soil and are often used for agriculture or settlements.

There are several types of valleys, including V-shaped valleys formed by erosion from rivers, U-shaped valleys carved by glaciers, rift valleys formed by tectonic activity, and hanging valleys created when smaller tributary valleys flow into larger main valleys.

A valley is a low-lying area of land between mountains or hills, often with a river running through it. Valleys are typically shaped by water erosion or glaciers and can provide fertile land for agriculture and settlements. They also offer natural pathways for transportation and communication.

The Kathmandu Valley has experienced development due to its historical significance, being the center of ancient trade routes and civilization in Nepal. It is also the country's political and economic hub, attracting investment and infrastructure development. Additionally, its cultural and religious heritage has made it a popular tourist destination, further driving its growth and development.

Valleys are good for agriculture because they provide fertile land for farming. They also offer natural barriers and protection for communities from strong winds or flooding. Additionally, valleys can be scenic and attract tourists for recreational activities like hiking and sightseeing.

Narrow deep valleys are sometimes called canyons.

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a small valley riginally worn away by running water and serving as a drainageway after prolonged heavy rains is called a Gully.