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| Presentation on the topic "Ural Mountains". Presentation on the topic "Ural Mountains" Geography project brochure about the Ural Mountains |
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Mount Narodnaya MOUNTAIN PEOPLE is the highest peak (1895 m) of the Urals. Located on the border of Komi and Khanty-Mansiysk Autonomous Republic. district, Subpolar Urals. Discovered by geologist A.N. Aleshkov in 1927 during an expedition to the Northern Urals. The mountain range reaches its greatest width in this area. The terrain is characterized by an alpine type of relief with steep slopes and deep gorges. The abundance of glacial forms, the presence of carts and circuses, in the depths of which lakes lie. In the high-mountain zone there are flat-topped massifs. MOUNTAIN NARODNAYA is the highest peak (1895 m) of the Urals. Located on the border of Komi and Khanty-Mansiysk Autonomous Republic. district, Subpolar Urals. Discovered by geologist A.N. Aleshkov in 1927 during an expedition to the Northern Urals. The mountain range reaches its greatest width in this area. The terrain is characterized by an alpine type of relief with steep slopes and deep gorges. The abundance of glacial forms, the presence of carts and circuses, in the depths of which lakes lie. In the high mountain zone there are flat-topped massifs
Amethyst star A variety of quartz. The color is due to the structural admixture of Fe. A type of quartz. The color is due to the structural admixture of Fe. In China, bottles and small boxes were cut out of light amethysts. In the Middle Ages, amethyst was highly valued in the East and Europe, where it was considered preferable for decorating church items and priestly clothing. When consecrated to the rank of cardinal, the initiate was given a ring with an amethyst, which is why in Catholic countries the stone was called episcopal, pastoral, and in Rus', bishop's. In China, bottles and small boxes were cut out of light amethysts. In the Middle Ages, amethyst was highly valued in the East and Europe, where it was considered preferable for decorating church items and priestly clothing. When consecrated to the rank of cardinal, the initiate was given a ring with an amethyst, which is why in Catholic countries the stone was called episcopal, pastoral, and in Rus', bishop's.
Chrysolite Chrysolite is a transparent variety of the mineral olivine - a silicate of iron and magnesium. Chrysolite is a transparent variety of the mineral olivine - a silicate of iron and magnesium. The word “chrysolite” (that is, “golden stone”; Greek chrysos “golden”) existed already in ancient times. It is found in ancient texts dating back to the 3rd century. BC e. The word “chrysolite” (that is, “golden stone”; Greek chrysos “golden”) existed already in ancient times. It is found in ancient texts dating back to the 3rd century. BC e. Sometimes the stone is called the evening emerald, because under artificial light the yellow tint disappears, and the stone appears pure green. Sometimes the stone is called the evening emerald, because under artificial light the yellow tint disappears, and the stone appears pure green.
Topaz According to the Bible, topaz is one of the 12 biblical stones with which the linen bag ("confidant") of the High Priest was decorated when he worshiped Jehovah. According to the Bible, topaz is one of the 12 biblical stones with which the linen bag ("confidant") was decorated. High Priest when he performed worship to Jehovah
Jasper has been known to man since the Paleolithic era, when weapons and tools were made from it. Known to man since the Paleolithic era, when weapons and tools were made from it. Later, various jewelry and talismans began to be carved from jasper. In Eastern countries, jasper was considered a symbol of beauty, grace and wealth. In Ancient Greece, the stone served as a talisman against the evil eye for young mothers and babies. Hippocrates treated fever and epilepsy with jasper. With the spread of Christianity, it was believed that jasper consecrated in the church had magical properties. A.S. Pushkin wore a bracelet with green jasper, considering it an assistant in love affairs. Later, various jewelry and talismans began to be carved from jasper. In Eastern countries, jasper was considered a symbol of beauty, grace and wealth. In Ancient Greece, the stone served as a talisman against the evil eye for young mothers and babies. Hippocrates treated fever and epilepsy with jasper. With the spread of Christianity, it was believed that jasper consecrated in the church had magical properties. A.S. Pushkin wore a bracelet with green jasper, considering it an assistant in love affairs.
Slide 2 Ural! The supporting edge of the power, Its breadwinner and blacksmith, The same age as our ancient glory and the creator of our present glory... A. Tvardovsky Slide 3 Slide 4 Slide 5 Geographical position.The Ural Mountains stretch from the coast of the Arctic Kara Sea to the steppes of Kazakhstan. The length of the Ural Mountains from south to north is 2 thousand kilometers, and from west to east from 50 to 150 kilometers. In ancient times, the Ural mountains were called Riphean, and until the 18th century “stone belt” (translated from Turkic “Ural” means belt). The Urals have long been considered a natural border separating two parts of the world - Europe and Asia. The Ural Mountains are relatively low: only a few peaks reach a height of 1.5 thousand meters above sea level, and the highest of them (Mount Narodnaya) is 1895 meters. Slide 6 Russian platform Ural fold system West Siberian plate Slide 7 Slide 8 The Ural Mountains are located between different tectonic structures (Russian Platform and West Siberian Plate), which explains their formation. The Urals are separated from the Russian Platform by the Pre-Ural trough, consisting of sedimentary rocks (clay, sand, gypsum, limestone). The Ural Mountains were formed during the Paleozoic period, but in the Mesozoic they were almost completely destroyed. Certain parts of the Urals rose during the Neogene. But these folded-block Ural Mountains were also destroyed as a result of the influence of external forces (weathering and erosion). Slide 9 Parts of the Urals.Slide 10 Polar UralsThe northernmost part of the Urals consists of rocky placers (rocks and outcrops). The flora and fauna are quite scarce. Even mosses and lichens do not create a continuous cover. The most significant peaks are the mountains: Payer (1472 meters) and Konstantinov Kamen (492 meters). Slide 11 SubpolarUralThis part of the Urals is characterized by the highest ridge heights. Here traces of glaciation are visible quite clearly. Even the names of the mountains speak volumes about their pointed peaks (Blade Peak, Saber Mountain). The highest point of the Ural Mountains (Mount Narodnaya) is also located here. Stone peaks and mountain tundra in the lower part of the slope are replaced by taiga. The southern border of this part of the Urals is located at 64º north latitude. Slide 12 Mount Saber Slide 13 Northern UralsThe mountains here take on the character of a real ridge, quite high, rocky and completely treeless. To the south its slopes are covered with forest. The average height of the Northern Urals is about 900 meters. Numerous rivers originate on its slopes, forming tributaries of the Pechora and Kama in the west, and the Ob in the east. Slide 14 amethyst emerald Slide 15 Slide 16 mid-altitude mountains Hercynian folding ore minerals sedimentary minerals uplands of the Cis-Urals edge of the Russian Platform ore minerals foothills of the Trans-Urals edge of the West Siberian Plate Slide 17 Slide 18 Climate.Despite its rather small height, the Ural Mountains have a fairly significant influence on climatic conditions. They are the boundary between different climatic zones: the temperate continental climate of the East European Plain and the continental climate of Western Siberia. Atlantic air masses reach the western slope of the Urals, trying to overcome it, rise higher and cool. As a result, more precipitation falls in the western part of the Urals than in the eastern part (about 1.5-2 times). The temperature regime also has its own characteristics. In the western part of the Urals, winter is snowier and, accordingly, milder. In the east there is less snow, and frosts reach 45-50 ºС. View all slides Oslyanka, the highest peak of the Middle Urals. Height 1119 m. There are two versions of the origin of the name of the mountain. The name of the river is Oslyanka, from the ancient Russian word “ass” - a whetstone, a river sharpening stone. The shape of the mountain, from the word “oslyad” or “osledina” - log. The mountain extends meridionally for 16 km. The ridge is leveled, mostly wide; in places narrow, steep, rocky. Has several peaks; the main one is located in the central part of the mountain, shifted to the eastern slope, and has a cone-shaped shape. The slopes are steep; The northern and eastern slopes have the greatest steepness. In the northern half of the mountain there are rocky outcrops and weathering remains. The slopes are covered with kurums; Mountain terraces are developed on the ridge. Avalanches have been observed. It is composed of quartz and pale-spar-quartz quartzite-sandstones of Upper Proterozoic age. Located in the northeast of the Kizelovsky district of the Perm Territory; in the axial part of the Middle Urals, north of the Basegi ridge, east-southeast of the Nyarovsky Kamen mountain. |
1 million km². Length more than 2000 km, width from 40 km in the north to 150 km in the south. Start with o. Vaygach, stretch along the 60th parallel, pass into the Guberlinsky mountains, the Mugodzhary mountains, and end at the shore of the Aral Sea with the General Syrt plateau and the Turgai plateau. The border between Europe and Asia passes through the Urals. The mountains have a barrier position relative to the western transport of air masses. "width="640" 
200: emerald, amethyst, aquamarine, jasper, rhodonite, malachite, etc.), jewelry diamonds. "width="640" 
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