Mountains

The larger copper mines are open pit mines. Copper ore is blasted with explosives, and loaded onto transport vehicles by heavy equipment. The ore is taken to a processing plant where it is crushed, the copper is removed chemically, and smelted into ingots of metal.

A dry mount is a method of mounting photographs or paper onto a backing board using dry adhesive materials such as photo corners or double-sided tape. This technique allows for the image to be easily removed or changed without causing any damage. Dry mounting is often used in framing to give a clean and professional finish to artwork or photographs.

The Jura Mountains and the Zagros Mountains are examples of the fold mountains. The fold mountain is formed as a result of the effects if the folding on layers within the upper part of the crust of the earth.

This is not always true. However, it depends on the placement between the mountain/volcano, and the placement of the tectonic lines of the tectonic plates floating underneath the earth's surface.

Mount Everest is approximately 6.6 times higher than Blue Mountain Peak. Everest stands at 29,032 feet (8,849 meters) above sea level, while Blue Mountain Peak is 7,402 feet (2,256 meters) tall.

Mount Kilimanjaro is spelled as "K-I-L-I-M-A-N-J-A-R-O."

Mauna Kea last erupted around 4,500 years ago. It is currently considered dormant and not actively erupting.

The continued uplift of many major mountain ranges is primarily driven by tectonic forces, including the collision of tectonic plates and the resulting crustal compression. This process leads to the gradual uplift and building of mountain ranges over millions of years. Other factors like erosion and volcanic activity can also contribute to the shaping and growth of mountains.

The Sierra Nevada mountain range in the United States is an example of a fault-block mountain. This range was formed by the tectonic forces that caused the hanging wall to rise and the footwall to drop along a normal fault. The distinctive block-like shape of the Sierra Nevada is a result of this movement.

Mount St. Helens in Washington state, USA is an example of a volcanic mountain. It is an active stratovolcano that famously erupted in 1980, causing significant destruction to the surrounding area.

Sand Mountain in Georgia was formed through a combination of geological processes, including deposition of sand through wind and water erosion, and subsequent uplift and tectonic activity in the region. Over millions of years, these processes led to the accumulation of sand particles and the gradual formation of the sand mountain as we see it today.

An upwarped mountain is formed by the uplifting of large sections of the Earth's crust due to tectonic activity. This process can lead to the gradual creation of a mountain range over millions of years. Upwarped mountains typically have broad, gentle slopes and are not as sharp or rugged as mountains formed by other processes.

3 Rock Types of Western Cordillera!

- Metallic Minerals: found in igneous rock.

Ex. iron + silver

- Nonmetallic Minerals: some metamorphic and sedimentary

Ex. potash + asbestos + mica

- Energy Minerals: California = offshore. Utah + Colorado = oil shale. Ex. Petroleum, coal, natural gas.

See the related link - Minerals/ locality database

Mechanical weathering, specifically the process known as abrasion, occurs when only the size of a rock is changed. This process involves the physical breakdown of rocks into smaller pieces through the grinding and rubbing action of moving sediment or other rocks.

Due to a phenononon called the Dry Adiabatic Lapse Rate. Air at the higher altitudes of a mountain summit will expend due to lower atmospheric pressures. As air expands, it cools at a rate of 9.8 degrees Celsius for every 1000m risen above sea level.

Therefore, on the summit of Mt Snowdon, UK, 1024m high, you could expect the temperature to be around 10 degrees cooler than it would be at sea level at any given time.

In Germany, there are quite a few mountains. I would say there is a good amount. There is not as many mountains in Germany as there are in other countries, such as Russia. So, to answer your question, yes, there are mountains in Germany. Thank you for your time.

The leeward side of a mountain is termed as the drier side, as it is the side of the mountain that faces away from the prevailing winds and therefore receives less moisture. This process, known as the rain shadow effect, results in the leeward side being arid or semi-arid compared to the windward side that receives more precipitation.

they face a lot of challenges like no food and they will get cold made from paper83@live.com

They need to build sturdy houses and have equipment in case someone falls.

they need to get lots og gas

these volcanoes are the southernmost volcanoes of the cascade volcanic chain.

Mountains have two effects on precipitation. These are the rain shadow effect and the orographic effect. These both cause the type and amount of precipitation to change because the air is forced higher up.

The eruption of the Soufrière Hills volcano on Montserrat caused the destruction of the capital city of Plymouth and the southern half of the island. About two-thirds of the population was evacuated due to the damage caused by pyroclastic flows, ashfall, and volcanic gases. The economy of Montserrat suffered greatly as tourism and agriculture were severely impacted.

A fault block mountain occurs when rock layers are pulled from opposite directions, large blocks slide downward, creating peaks and valleys. See Link

edited by ERIC: To make it easier (SHEARING)

Mount Kosciuszko is made of granite rocks. It was formed in the Ordovician period and is 2228 meters tall at its highest point.