Valleys

Common flora in Monument Valley include desert plants like sagebrush, pinyon pine, and juniper trees. Wildlife in the area includes desert species such as coyotes, mule deer, and various birds like ravens and hawks.

A central valley is a elongated valley that is typically found between mountain ranges. It is often characterized by flat or gently rolling terrain, and is commonly used for agricultural purposes due to its fertile soil and access to water sources. Examples include the Central Valley in California and the Great Rift Valley in Africa.

It is well known for having large amounts of human fossils wich scientist have found very usefull in their studies.

for more information go to the related links box below to read the wikipedia riff valley article.

V-shaped valleys are typically formed by the continuous erosion of flowing water over a long period of time. The erosion occurs through the processes of hydraulic action, abrasion, and corrosion, which gradually wear away the surrounding rock and soil, creating the characteristic V-shape. This erosion is often accelerated by factors such as tectonic activity, glaciation, or human interference.

Some of the valleys in Trinidad and Tobago include Maracas Valley, Caura Valley, Santa Cruz Valley, and Chaguaramas Valley. These valleys are known for their lush vegetation, diverse wildlife, and picturesque scenery, attracting visitors and nature enthusiasts.

The term "valley walls" is metaphorical; valleys do not actually have walls, they have hills. Valleys are between hills, that's why they are valleys. If there were no hills, the valley would just be a plain.

A tributary valley that joins a main valley where the latter has been deepened, usually by glacial erosion, resulting in a steep drop from the floor of the tributary valley to the floor of the main valley. For the source and more detailed information concerning this subject, click on the related links section (Answers.com) indicated below this answer box.

The sides of the valley heating more quickly than the air around it

The climate in the Great Rift Valley varies depending on the specific location within the region. Generally, it has a diverse climate with some areas experiencing tropical wet conditions while others have more arid or semi-arid climates. The highland areas can be cooler with more rainfall, while the valley floor tends to be hotter and drier.

The Jordan River Valley is located in the Middle East, flowing through Israel, Jordan, and the Palestinian territories. It is a historically significant region, known for its role in biblical events and its importance in the geopolitics of the area.

The first civilations arose in river valleys because good farming conditions made it easy to feed large numbers of people. The rivers also made it easy for people to go from place to place to trade.

The Barossa Valley in Australia is famous for the production of high-quality wine, particularly Shiraz and other red varietals. The region's unique climate and soil conditions have helped establish it as a world-renowned wine region.

Moon valleys are geological formations typically found in arid or desert regions, characterized by unique landscapes with deep valleys, sharp ridges, and unique rock formations. They get their name from their resemblance to the surface of the moon due to their desolate and otherworldly appearance. Moon valleys are often popular tourist destinations known for their natural beauty and geological significance.

V-valley refers to a type of valley on a topographic map that has a V-shaped profile, typically formed by erosion from a river or stream. U-valley refers to a valley with a U-shaped profile, typically formed by glacial erosion. V-valleys are more narrow and have steeper sides compared to U-valleys.

The Great Rift Valley is located in East Africa, stretching from the region of the Dead Sea in the Middle East to Mozambique in Southern Africa. It runs through several countries including Ethiopia, Kenya, and Tanzania.

A long valley profile shows the cross-sectional view of a valley from its headwaters to its mouth. It typically displays the variations in elevation and slope along the length of the valley, often revealing features such as V-shaped valleys, interlocking spurs, and river meanders. This profile is useful for analyzing the geological and geomorphological history of a valley.

The Valley of the Kings is located at an elevation of about 420 meters (1,378 feet) above sea level.

The Napa Valley is located about an hour north of San Francisco. The Valley is 30 miles long and ranges from 1 to 5 miles in width. This is one of the top wine producing regions of the world and attracts many visitors. There are more than 200 wineries with tasting rooms where you can visit and sample the wines. Many provide tours.

There are several ways. It depends on what sort of mountain your talking about.

Mountains form due to the movement of tectonic plates under the earths crust. for example there is a compresional plate boundary where the plates move together. --><--

This will form a cone mountain/volcano. Mountains can also form from erosion or water. If a stream is created, then after years it will disintegrate dirt and could leave a higher mound, which over a large amount of time, could create a mountain.

Valleys are typically formed by a combination of erosion processes such as rivers cutting through the land, glaciers carving out U-shaped valleys, or tectonic forces creating fault-block valleys. Over time, these processes shape the landscape by wearing away the Earth's surface, leaving behind the characteristic V-shaped valleys we see today.

Rift Valleys and divergent boundaries occur where two tectonic plates are spreading apart. A good example of a Rift Valley is the one located in Africa between Somalia and Ethiopia.

Yosemite Valley in California is a famous example of a valley. It is located within Yosemite National Park and is known for its towering granite cliffs, waterfalls, and lush meadows.

The cohesive forces between liquid molecules, such as hydrogen bonding or van der Waals forces, hold liquids together. These forces create a surface tension that allows liquids to maintain a compact shape and form droplets.

Valley glaciers are streams of flowing ice that are confined by steep walled valleys, often following the course of an ancient river valley. They usually form from Cirques, where the glacier overspills the hollow and begins to travel down the valley. Alternatively, they may form branching off from an ice sheet. The downward erosive action of the ice carves a U shaped valley, as opposed to a V shaped valley for rivers. They have a lot of erosive potential as they are thick bodies of ice exerting extreme amounts of pressure. Valley glaciers 'choose' the most accessible route and erode and enlarge the area. It uses erosional processes, plucking and abrasion. Due to the size and nature of the glacier it can pick up large amounts of debris and scree and deposits it as moraine.