Mountains

Leeward - the moisture gets wrung out on the windward side when the air is forced to rise and cool and condense into clouds and precipitation. There isn't much left for the leeward side, particularly given that the air tends to sink.

The Ring of Fire is a horseshoe-shaped area in the Pacific Ocean known for its high seismic and volcanic activities. It is home to about 75% of the world's active and dormant volcanoes. The region experiences frequent earthquakes and volcanic eruptions due to the movement of tectonic plates along the boundaries.

The eruption of Mount Vesuvius in 79 AD was caused by the subduction of the African Plate beneath the Eurasian Plate. This collision led to the formation of magma chambers beneath the Earth's surface, eventually resulting in the catastrophic eruption that buried the cities of Pompeii and Herculaneum.

Diamond Head, a volcanic tuff cone on the island of Oahu in Hawaii, last erupted around 300,000 years ago. Its formation is linked to a series of volcanic events that took place over thousands of years in the region.

Volcanoes occur most commonly along tectonic plate boundaries, such as the Ring of Fire around the Pacific Ocean. This is where plates either collide, move apart, or slide past each other, resulting in volcanic activity. Additionally, volcanoes can also form in hotspots, where a plume of magma rises from deep within the Earth's mantle.

The most recent eruption of Mount Vesuvius occurred in 1944, causing significant damage to surrounding towns and infrastructure. The estimated economic damage from this eruption was around $100 million at the time.

Mt Etna erupted due to the movement of magma from the Earth's mantle towards the surface through the volcano's vent. This process caused pressure to build up within the volcano, eventually leading to an eruption. Magma is formed through the melting of rock beneath the Earth's surface, and when it rises towards the surface, it can result in volcanic activity.

It is spelled Kosciusko, and it is located in Australia. It is also Australia's tallest mountain.

A lifted mountain is a mountain that formed due to both volcanic activity and earth movement which made sure that the compression of two landmasses pushed some land upwards. There is involvement of seismic activity.

Lookout Mountain is a type of landform known as a mountain, characterized by its steep elevation and prominence above the surrounding area. It often offers panoramic views from its summit due to its height.

We can divide the effects of an earthquake into those known as the primary effects and those known as the secondary effects. Primary effects of an earthquake are those resulting directly from the earthquake itself. These include; buildings collapsing; roads cracking; bridges giving way; shattering of glass and injuries / deaths resulting from these. Secondary effects are those that result from the primary effects. For example ground shaking may result in the cracking of gas and water pipes (primary effects) this can result in severe fires due to explosion from escaping gas and difficulties in putting out fires due to lack of water from burst mains (secondary effects). Other secondary effects include, homelessness, business going bankrupt and closing etc.

Monadnock is an originally Native American term for an isolated hill or a lone mountain that has risen above the surrounding area, typically by surviving erosion. The name was taken from Mount Monadnock in New Hampshire (USA). The name is thought to derive from the Abenaki language, from either menonadenak ("smooth mountain") or menadena ("isolated mountain").

The collision of the Indian Plate with the Eurasian Plate led to the creation of the Himalayan Mountains. The Indian Plate is moving northward towards the Eurasian Plate, causing the two plates to collide. The immense pressure and force from this collision led to the uplift and formation of the Himalayas.

name three volcanic mountains in Washington

A streak test involves rubbing a mineral against an unglazed porcelain plate to see the color of the streak left behind, which can help identify the mineral. The color of the streak is often more consistent and reliable than the color of the mineral itself.

A volcano is a mountain from which lava flows out during an eruption.

There are many active volcanoes around the world, which means it may erupt in the near future. Some of these include Kilauea Volcano, Hawaii, San Salvador, El Salvador, as well as Merapi Volcano, Java, Indonesia.

nothing some people died some lived others just carried on with life and till then nothing amazing happened to their lives except they died and went to hell and heaven and thier children carried on their families for them because they are "nice and good people" but messed up tooo lol

when a colliding boundary collides and pushes up a mountain. an example of a fault block mtn. range is the Himalayas.

Actually the previous answer is incorrect. They form when the tenison pu on Earth is so great that it caused large blocks of rock to move down relative to the other causing a change in elevation and a moutain to form. The previous answer was how folded mountains form....

Mount Vesuvius in Italy has an elevation of 1,281 meters (4,203 feet) above sea level.

Yes, because its part of the earth and its stable, doesnt change or go away its not like a building.

Mount Tarawera last erupted in June 1886. The eruption caused significant damage to the surrounding area and claimed many lives.

A fault-block mountain is characterized by steep, rugged slopes on one side and a more gradual slope on the other. They are formed when tectonic forces cause a block of rock to be uplifted along a fault line, creating a mountain range with distinct asymmetric features. Examples include the Sierra Nevada in California and the Teton Range in Wyoming.

Yes, mountains are considered abiotic, meaning they are non-living components of an ecosystem. Mountains are comprised of rock, soil, water, and air, which are all abiotic factors that influence the environment and support various forms of life.

The Zagros Mountains span from approximately 32°N to 37°N latitude and 44°E to 48°E longitude, covering parts of Iran, Iraq, and Turkey.