Names of low mountains up to 1000 meters. Relief of the Earth

What low mountains are there? Name and height! Up to 1000 m and got the best answer

Answer from Amazon[guru]

The low-mountain regions of Kazakhstan include Saryarka (500-600m), Mugodzhary (the highest place is Bolshoy Boktybai 657 m). and Mangystau Mountains. The highest point of the Mangystau Mountains in the Karatau ridge is Besshoky (556 m).

Answer from Marina[newbie]
LOW MOUNTAIN TYPE OF RELIEF, Low mountains - the relief of low (up to 1000 m) mountains, characterized by predominantly soft outlines and usually distributed along the periphery of mountainous countries.
Mountain ranges of the North-Western Caucasus, Middle Urals and Khibiny.
Świętokrzyskie Mountains: the oldest and the lowest - the highest mountain Łysica rises only 612 m above sea level

Answer from Polina Bespalova[newbie]
LOW MOUNTAIN TYPE OF RELIEF, Low mountains - the relief of low (up to 1000 m) mountains, characterized by predominantly soft outlines and usually distributed along the periphery of mountainous countries.
Mountain ranges of the North-Western Caucasus, Middle Urals and Khibiny.
Świętokrzyskie Mountains: the oldest and the lowest - the highest mountain Łysica rises only 612 m above sea level
The low-mountain regions of Kazakhstan include Saryarka (500-600m), Mugodzhary (the highest place is Bolshoi Boktybai 657 m). and Mangystau Mountains. The highest point of the Mangystau Mountains in the Karatau ridge is Besshoky (556 m).

Answer from 3 answers[guru]

Hello! Here is a selection of topics with answers to your question: What low mountains are there? Name and height! Up to 1000 m.

What is absolute and relative height?

Absolute height – the height of a geographical object relative to sea level.

Relative height is the elevation of one point on the earth's surface above another.

Where are mountains formed?

Mountains are formed at the junction of two lithospheric plates, where layers of rocks are crushed into folds.

Locate the Andes Mountains on a map and determine their extent from north to south.

The length of the Andes is 9000 km.

What is the height of Chomolungma? Find the Caucasus Mountains on the map and name the height of Elbrus.

The height of Chomolungma is 8848 m. The height of Elbrus is 5642 m.

What external processes operate on the land surface?

Processes of physical, chemical and biological weathering operate on the land surface.

Questions and tasks

1. What is the difference between mountains and plains?

Mountains and plains differ in absolute heights and variations in heights. Mountains are characterized by high absolute heights and their sharp changes, i.e. mountain ranges alternate with intermountain depressions. Plains are characterized by a relatively flat surface with low absolute heights.

2. How do mountains differ in height? Give examples of mountains of different heights.

Based on absolute height, mountains are divided into three groups: low - below 1000 m (Middle Urals), medium - from 1000 to 2000 m (Carpathians) and high - above 2000 m (Himalayas).

3. How do plains differ in height? Give examples of plains of different heights.

Plains with a height of 0 to 200 m above sea level are called lowlands (Caspian lowland, Amazonian lowland), from 200 to 500 m (East European Plain) are called uplands, and above 500 m are called plateaus (Central Siberian Plateau).

4. How do mountains change over time?

Vertical movements of the earth's crust raise the ridges upward, and external processes tend to destroy them. The mountains are gradually decreasing, the slopes are becoming flatter, and the river valleys are expanding. High mountains turn first into low ones, then into a plain.

5. Using physical maps of the world and Russia in the atlas, find, show and name the lowlands, hills and plateaus located on the Eurasian continent and on the territory of our country. Using the altitude scale, determine the highest altitude characteristic of the Central Siberian Plateau.

Lowlands of Eurasia - Caspian, Black Sea, Pechora, West Siberian, Turanian, Indo-Gangetic.

Hills - Valdai, Central Russian, Volyn-Podolsk, Volga, Smolensk-Moscow.

Plateau – Central Siberian, Deccan.

The highest point of the Central Siberian Plateau is Mount Kamen - 1800 m.

6. Using the physical map of Russia, determine which mountains surround the East European Plain. Which ones are high, and which ones are medium and low?

In the northwestern part it is limited by the mountains of Scandinavia, in the southwestern part by the Sudetes and other mountains of central Europe, in the southeastern part by the Caucasus, and in the east by the Urals. The Caucasus is high mountains. The Sudetes are low mountains. Ural - middle mountains.

7. Using a physical map of the hemispheres, determine which continent is the most mountainous and which is the flattest?

Eurasia is the most mountainous continent. Australia is the flattest continent.

What low mountains are there? Name and height! Up to 1000 m and got the best answer

Answer from 3 answers[guru]

Hello! Here is a selection of topics with answers to your question: What low mountains are there? Name and height! Up to 1000 m.

Classification of mountains by height - medium (height m) Ural

The Ural Mountains are a mountain system between the East European and West Siberian plains. The length of the Ural Mountains is more than 2000 km, width from 40 to 150 km. In ancient sources, the Ural Mountains are called the Riphean or Hyperborean Mountains. Russian pioneers called it Stone. The name Ural comes from the Mansi "ur" (mountain). The Ural Mountains were formed in the late Paleozoic during an era of intense mountain building (Hercynian folding).

Mount Narodnaya is the highest peak (1895 m) of the Urals. Discovered by geologist A.N. Aleshkov in 1927. The mountain itself, except for its height, does not stand out against the background of the surrounding mountains of the Subpolar Urals. It is characterized by the presence of carrs and cirques, in the depths of which lakes lie. There are glaciers and snowfields.

M o r a e r m a k rock massif (mountain), located in the Kungur region, Perm region. The Sylva River flows at the foot. The rock is composed mainly of limestones. Ermak has three peaks, Ermak, Ermachikha, Ermachenok, all of them have different heights. There is a cave in the mountain. The legend says that in ancient times Ermak Timofeevich spent the winter in this cave and allegedly hid a treasure there. The Ermak stone is a very popular place for tourists.

VETLAN The Vetlan stone is a rocky outcrop on the Vishera River, near the city of Krasnovishersk in the Perm region. Since 1981 it has been a protected landscape of regional importance. The stone is an almost vertical wall stretching along the Vishera River for 1750 meters. The height of the rocks reaches 100 meters. In the area of the Vetlan stone, a large number of different plants grow, 15 of which are listed in the Red Book.

Volchikha Volchikha is the highest mountain in the vicinity of Yekaterinburg (height 526m). The mountain is located near the cities of Pervouralsk and Revda. The rocky peak of Volchikha rises above the forest. In the direction of Revda and Pervouarlsk, in calm weather, the valley at the foot of the mountain is clearly visible. The Volchikha Reservoir and the bends of the Chusovaya River are also clearly visible. You can also see the peak of Belaya (527m.)

Mountains vary in height, shape, age, origin, geographical location, etc. The article provides a description of the listed types of mountains.

Mountains by height

Lowlands

Low mountains or low mountains - mountain heights up to 800 meters above sea level.

Peculiarities:

The tops of the mountains are round, flat,
The slopes are gentle, not steep, covered with forest,
Characteristically, there are river valleys between the mountains.

Examples: Northern Urals, spurs of the Tien Shan, some ridges of Transcaucasia, Khibiny Mountains on the Kola Peninsula, individual mountains of Central Europe.

Srednegorye

Middle mountains (medium or mid-altitude mountains) - the height of these mountains is from 800 to 3000 meters above sea level.

Medium-altitude mountains are characterized by altitudinal zonation, i.e. change of landscape with change in altitude.

Examples of medium mountains: Mountains of the Middle Urals, Polar Urals, mountains of the island of Novaya Zemlya, mountains of Siberia and the Far East, mountains of the Apennine and Iberian Peninsulas, Scandinavian mountains in northern Europe, Appalachians in North America, etc.

Highlands

Highlands (high mountains) - the height of these mountains is more than 3000 meters above sea level. These are young mountains, the relief of which is intensively formed under the influence of external and internal processes.

Peculiarities:

The mountain slopes are steep, high,
The peaks of the mountains are sharp, peak-shaped, and have a specific name - “Carlings”,
The mountain ridges are narrow, jagged,
It is characterized by altitudinal zones from forests at the foot of the mountains to icy deserts at the tops.

Examples: Pamir, Tien Shan, Caucasus, Himalayas, Cordillera, Andes, Alps, Karakoram, Rocky Mountains, etc.

Mountains by shape

According to the nature of the summit endings, mountains are: peak-shaped, dome-shaped, plateau-shaped, etc.

Peaked mountain peaks

Peaked mountains are pointed mountain peaks that are shaped like peaks, hence the name of this type of mountain peak. They are characteristic mainly of young mountains with steep rocky slopes, sharp ridges and deep crevices in river valleys.

Examples of mountains with peaked peaks:

Peak Communism (mountain system - Pamir, height 7495 meters)
Pobeda Peak (Tian Shan mountain system, height 7439 meters)
Mount Kazbek (mountain system - Pamir, height 7134 meters)
Pushkin Peak (mountain system - Caucasus, height 5100 meters)

Domed mountain peaks

The dome-shaped, that is, rounded, shape of the top can be taken by:

Laccoliths are unformed volcanoes in the form of a hill with a magma core inside,
Extinct ancient heavily destroyed volcanoes,
Small areas of land that have undergone a dome-shaped tectonic uplift and, under the influence of erosion processes, have taken on a mountainous appearance.

Examples of mountains with a dome-shaped peak:

Black Hills (USA). The area was subject to dome uplift and much of the sedimentary cover was removed by further denudation and erosion. As a result, the central core was exposed. It consists of metamorphic and igneous rocks.
Ai-Nikola (Ukrainian Ai-Nikola, Crimean tat. Ay Nikola, Ai Nikola) is a domed outlier mountain, the southeastern spur of Mount Mogabi near the western outskirts of the village of Oreanda. It is composed of Upper Jurassic limestones. Height - 389 meters above sea level.
Kastel (Ukrainian Kastel, Crimean Catholicate. Qastel, Kaastel) is a mountain 439 m high on the southern outskirts of Alushta, behind the Professor’s Corner. The dome of the mountain is covered with a forest cap, and chaos has formed on the eastern slope - boulders of stone, sometimes reaching 3-5 m in diameter.
Ayu-Dag or Bear Mountain (Ukrainian Ayu-Dag, Crimean Catholicate. Ayuv Dağ, Ayuv Dag) is a mountain on the southern coast of Crimea, located on the border of Big Alushta and Big Yalta. The height of the mountain is 577 meters above sea level. This is a classic example of a laccolith.
Kara-Dag (Ukrainian Kara-Dag, Crimean Catholicate. Qara dağ, Kаara dag) is a mountain-volcanic massif, Crimea. Maximum height - 577 m (Mount Holy). It is a heavily destroyed volcanic form with a dome-shaped top.
Mashuk is a remnant magmatic mountain (laccolith mountain) in the central part of Pyatigorye on the Caucasian Mineral Waters, in the northeastern part of the city of Pyatigorsk. The height is 993.7 m. The peak has a regular dome shape.

Plateau-shaped mountain peaks

Mountain peaks that are flat in shape are called plateau-shaped.

Front Range Front Range) is a mountain range in the southern part of the Rocky Mountains in the United States, adjacent to the Great Plains on the west. The ridge stretches from south to north for 274 km. The highest point is Mount Grays Peak (4349 m). The ridge is composed mainly of granites. The peaks are plateau-shaped, the eastern slopes are gentle, the western slopes are steep.
Khibiny (Kild. Umptek) is the largest mountain range on the Kola Peninsula. Geological age is about 350 million years. The peaks are plateau-shaped, the slopes are steep with isolated snowfields. However, not a single glacier was discovered in the Khibiny Mountains. The highest point is Mount Yudychvumchorr (1200.6 m above sea level).
Amba (translated from Amharic as Mountain Fortress) is the name of the flat-topped hills and mesas in Ethiopia. They consist mainly of horizontal sandstones and layers of basalt. This determines the flat-topped shape of the mountains. Ambas are located at an altitude of up to 4,500 m.

Mountains by age

By age, mountains are divided into:

Young mountains,
Old (ancient) mountains.

Young mountains formed over the last 50 million years. In these mountain systems, internal processes are very actively developing, accompanied by the formation of mountains, earthquakes, and sometimes even volcanic activity. The youngest mountains on Earth are those belonging to the continental and island rings of the Pacific Ocean. The Caucasus Mountains are recognized as the youngest mountains in Russia. Here is the highest mountain in Russia - Elbrus (5642 m). (In the picture on the left: The Himalayas are young mountains, geological age about 38 million years)

Features of the young mountains:

the process of growth of young mountains is still ongoing,
the relief is sharp, highly dissected,
the peaks of the ridges are sharp,
the mountain slopes are steep and high,
high absolute altitudes,
significant height amplitude,
the valleys of numerous rivers are presented in the form of gorges, gorges,
Young mountains are characterized by the development of glaciers.

Examples of young mountains are:

Alps,
Caucasus Mountains,
Carpathians,
Kopet-Dag,
Pamir,
Mountains of Kamchatka.

Old (ancient) mountains are several hundred million years old. They differ in that the internal processes in them have long since died down, while the external processes that influence the destruction of the mountains are still active. This will continue until the relief is completely leveled. On many modern plains there are areas where, by all indications, there were once ancient mountains. From these mountains, only roots remained in the depths, covered with a thick layer of sedimentary rocks.

Features of old (ancient) mountains:

were heavily damaged,
have less contrasting relief,
the elevation differences are small,
gentle slopes,
The river valleys are well developed.

Examples of old (ancient) mountains are:

Ural mountains,
Timan,
Yenisei Ridge,
Khibiny (Kola Peninsula, geological age approximately 350 million years).

By origin

Tectonic mountains are formed as a result of the collision of moving sections of the earth's crust - lithospheric plates. This collision causes folds to form on the surface of the earth. This is how folded mountains arise. When interacting with air, water and under the influence of glaciers, the rock layers that form folded mountains lose their plasticity, which leads to the formation of cracks and faults. Currently, folded mountains have been preserved in their original form only in certain parts of the young mountains - the Himalayas, formed during the era of Alpine folding.

With repeated movements of the earth's crust, hardened folds of rock are broken into large blocks, which, under the influence of tectonic forces, rise or fall. This is how folded block mountains arise. This type of mountains is typical for old (ancient) mountains. An example is the Altai mountains. The emergence of these mountains occurred during the Baikal and Caledonian eras of mountain building; in the Hercynian and Mesozoic eras they were subject to repeated movements of the earth's crust. The type of folded-block mountains was finally adopted during the Alpine folding.

Volcanic mountains are formed during the process of volcanic eruptions. They are usually located along fault lines in the earth's crust or at the boundaries of lithospheric plates.

There are two types of volcanic mountains:

Volcanic cones. These mountains acquired their cone-shaped appearance as a result of the eruption of magma through long cylindrical vents. This type of mountain is widespread throughout the world. These are Fuji in Japan, Mount Mayon in the Philippines, Popocatepetl in Mexico, Misti in Peru, Shasta in California, etc.
Shield volcanoes. Formed by repeated outpouring of lava. They differ from volcanic cones in their asymmetrical shape and small size.

In areas of the globe where active volcanic activity occurs, entire chains of volcanoes can form. The most famous is the chain of Hawaiian Islands of volcanic origin, more than 1600 km long. These islands are the tops of underwater volcanoes, whose height from the surface of the ocean floor is more than 5500 meters.

Erosion (denudation) mountains

Erosion mountains arose as a result of the intensive dissection of stratified plains, plateaus and plateaus by flowing waters. Most mountains of this type are characterized by a table shape and the presence of box-shaped and sometimes canyon-type valleys between them. The last type of valley occurs most often when a lava plateau is dissected.

Examples of erosional (denudation) mountains are the mountains of the Central Siberian Plateau (Vilyuisky, Tungussky, Ilimsky, etc.). Most often, erosion mountains can be found not in the form of separate mountain systems, but within mountain ranges, where they are formed by the dissection of rock layers by mountain rivers.

By geographical location

On this basis, it is customary to group mountains into mountain systems, ridges, mountain ranges and single mountains.

Mountain belts are the largest formations. There are the Alpine-Himalayan mountain belt, stretching across Europe and Asia, and the Andean-Cordilleran mountain belt, passing through North and South America.

Mountainous country - many mountain systems.

Mountain system - mountain ranges and groups of mountains that are similar in origin and have the same age (for example, the Appalachians)

Mountain ranges are interconnected mountains stretched out in a line. For example, the Sangre de Cristo Mountains (North America).

Mountain groups are also mountains connected to each other, but not elongated in a line, but forming a group of indefinite shape. For example, Mount Henry in Utah and Bear Paw in Montana.

Solitary mountains are mountains that are not connected to other mountains, often of volcanic origin. For example, Mount Hood in Oregon and Rainier in Washington.