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#учебниквслух

аудио уроки

школьный учебник

география

8 класс

домогацких

тектоническое строение

строение земной коры

тектонические карты

складчатые пояса

структурные части платформы

евразиатская литосферная плита

складчатый пояс

осадочный чехол

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grade lesson topic

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tectonic structure almost the entire

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territory of our country is located within the

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Eurasian lithospheric plate this

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plate occupies a huge area and Russia

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occupies only part of it borders

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lithospheric plates mostly lie

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far from the borders of our country

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several adjoin the Eurasian plate

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plates large North American

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Pacific relatively small

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willingly Morskaya and Amur

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there are complex and diverse

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processes associated with the collision and

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rarefaction of lithosphere blocks the

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rest of the country's territory is

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geologically

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relatively calm, however this was not

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always the case in geological history there were

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periods when

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significant geological events took place on the territory of Russia

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In the Proterozoic, the

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territory of the modern Central Siberian

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plateau was broken up by a system of

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deep wrinkles along which

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mantle material rushed to the surface of the earth for many

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millions of years,

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almost continuous

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volcanic eruptions continued over a huge area, traces of these

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eruptions can be traced even in the

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modern topography, the plateau

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began to move in the Carboniferous period 2 lithospheric plates

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that formed the modern

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Eurasian one, as a result, on their

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border a huge mountain

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range was formed in height almost equal to

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modern ones, quite a few of them

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where it now stands in the same place where it

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arose only weathering forces

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completely changed its appearance in place of snow-

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capped peaks rising to the very clouds,

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now low heavily destroyed mountains of

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Uralsk

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in the Mesozoic, a vast area of land

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lying east of the Urals sank

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two to three kilometers and in place of the

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West Siberian Plain there was a huge

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sea to characterize the history of the

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formation and structure of the earth's crust,

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tectonic maps are used, these

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maps depict the main elements of the

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structure of the earth's crust tectonic

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structures the main tectonic

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structures are platforms and

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folded belts

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platforms are large two to three thousand

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kilometers in diameter relatively

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stable sections of the earth's crust

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once in place of the platforms there were mountains under the

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influence of weathering forces and did not

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collapse the earth's surface

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was leveled and layers were deposited on it

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sedimentary rocks clay sands

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limestones

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how in place of the folded belt

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platforms are formed and the mountains are replaced by

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plains the structure of the platforms there are

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two tiers the lower tier

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is a base called the

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foundation or base layers of

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rocks in the base of the platform mortal

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folds are the remains of those same folded

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choir that were here before the upper a

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layer of sedimentary rocks is called a

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sedimentary cover; it is thicker than rocks,

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most often of clastic origin,

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which cover the earth's surface,

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hiding the unevenness of the base. According to the age of the

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foundation, the platforms are divided into ancient and

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young; in ancient platforms, the foundation was

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formed in the Warfare and

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Proterozoic eras; in young

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platforms, in the Paleozoic era, the relief

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there are vast plains,

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each tier of the platform has

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its own minerals, the folded

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foundation

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most often contains a variety of ores, and

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in the sedimentary cover, oil, gas, coal, salts and

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other fossils of sedimentary

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origin, the surface of the folded

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base of the platforms is uneven, so the

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depth of occurrence of its individual parts

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varies depending on the depth of

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occurrence on the platforms. shields and

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slabs extensive outcrops of the

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platform foundation to the surface are called

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abacus within the abacus

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very ancient rocks

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that never lay at the base of the mountains come to the surface the

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lowered parts of the platform foundation

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covered with a thick sedimentary cover

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several kilometers thick are called

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slabs in the tectonic structure of Russia

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several large abacus can be distinguished

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and plates last year we talked

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about the eras of mountain building or

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folding,

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the territory of our country, like the whole

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earth, has gone through several such eras, the mountains

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formed in one or another era of

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folding have different ages, the

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area of the most ancient folding

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which occurred in the Harp and part of the

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Proterozoic era occupies a huge

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territory of our country,

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mountains of this age are, of course, long gone,

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since they arose more than a billion

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years ago and were completely destroyed by weathering forces.

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rocks of this age form the

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foundation of the ancient platforms of the country. In

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some places, these ancient

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rocks of a folded base reach the

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surface of the earth. In these places there

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are large shields Baltic

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Aldan

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and Anabar at the beginning of the Paleozoic

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continued bureau formation that

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began in the Proterozoic ska and time this

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period is called the Baikal

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folding and there were few traces left

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throughout the first half of the Paleozoic

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era went to the Lydon ska and mountain building

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which in the second half of the era was replaced by the

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Herzensky as a result of the Koli Donskoy

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300 million years ago and the Kerch

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150 million years ago, folding

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between the ancient platforms formed

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mountains, these ancient mountains were gradually

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destroyed, but in the Cenozoic

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they were uplifted and younger than now, new

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mountains formed at the beginning of the Mesozoic

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in the northeast of Eurasia, a

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mobile folded belt of the Mesozoic arose,

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and at first a depression of the earth's crust arose

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and large areas were occupied by milka

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water seas at the end of the Cretaceous period, the

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subsidence of the land surface gave way to

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an ascent, which led to the formation of

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several large mountain systems in

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Siberia and in the Far East a

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number of mountain systems arose: the Verkhoyansk

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ridge, the Chersky ridge, the ridges of Chukotka and

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Sikhote-Alin

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in the region of Cenozoic folding in

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Russia includes the

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Alpine in the south and the Pacific in the

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east according to iso, although the Alpine

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belt

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includes a relatively small region of

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Russia, the Caucasus and Crimean mountains

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formed about 5-10 million years

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ago in the Pacific belt, the Pacific

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Ring of Fire

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which borders the ocean on almost all

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sides in within Russia includes the mountains

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of Kamchatka, Sakhalin and the Kuril Islands,

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mountain building continues here and in

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our time it is accompanied by strong

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earthquakes and frequent

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volcanic eruptions. Let us repeat the main thing in the

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tectonic structure of Russia, there are

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sections of the ancient Eastern European and

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Siberian

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and young western

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mountain and Pechora platforms occupying

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most of the country's territory

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folded belts of different ages

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separate and surround the platform

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areas of the

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Russian mountains; they were formed in different eras

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of folding; the

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oldest mountains in the country are located in the

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Baikal region,

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and the youngest are in the Far East

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