Presentation to the lesson in geography (grade 5) on the topic: Presentation "Local Orientation".

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Which device will help us determine the parties of the horizon?

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Initially, people defined the side of the sunrise.

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On the lunar night, during the full moon, the moon is at 19 o'clock - in the east, at 1 o'clock in the morning - in the south and at 7 o'clock in the morning - in the West (Fig. 48).

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But how to be when the moon is not visible?

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The observer should be well remembered on the area direction to the north, in order to be able to be able to specify the side of the horizon without a compass, for memory.

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The fastest is the method of determining the Sun and the clock;

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{!LANG-ade6369d4e2b7cfc7b92ecc82ed74fb3!} Refined method of orientation on the Sun and Clock

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However, the situation may be such that due to the cloudiness there is no big bear, nor the polar star, but can be seen moon.

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A dividing line passing between it division, the center of the clock and the number "1".

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Here we will see such constellations as Orion, Taurus, Gemini, Leo, Swan.

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In November, the Constellation of the Taurus, depicted from fig.

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The resulting number will indicate an approximate time.

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Arrows can also serve as stars of other constellations close to the polar star, but the coefficients in such cases will be other numbers.

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The overwhelming majority of features are associated with the position of objects with respect to the Sun.

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In the polar night in the Arctic - the picture is the opposite: the most light part of the sky is South, North - the most dark.

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Quarter numbers are noted on the so-called quarterly pillars exhibited at all intersections.

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On the slopes addressed to the south, in the spring are gasy appear the faster than the cooler of these slopes: each extra degree of slope of the area to the south as it was equivalent to the approximation of the terrain one degree to the equator.

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It is noticed that in many mountainous areas of Siberia slopes facing south, more detached, as they are previously exempted from snow, they used to die and lighten to be destroyed by raindrops and snowy waters.

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It is possible to judge the direction of the dominant wind at the inclination of the centers of most trees, especially on the edges and separate trees, whose slope is more noticeable;

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In the mountains, steppes and tundra, dominant winter winds, moving snow (blizzards, Purga), have a great influence on the terrain.

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As a result of the movement of snow, various surface formations are created in the form of transverse and longitudinal snow accumulations with respect to the wind.

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Their atmosphere slopes are sealed with wind, the sands are tightly pressed by one to the other;

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In the Australian deserts, sand ridges are pulled in the form of many parallel to each other weakly winding lines separated by one from another distance on average about 400 m. These ridges reaches lengths of several hundred kilometers.

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In the mountains of the Western Caucasus on the southern slopes, pine grows, on the northern - beech, spruce, fir.

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* * *

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Bubnov I., Krepe A., Folimonov S.,

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"GEF lesson" - GEF.

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Building "Rose Winds" is necessary for the arrangement of the runways of aerials, when building residential areas in relation to industrial zones (calculation of the probability of demolition by the air masses of harmful emissions from enterprises), roads.

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Stage "Check Home Task"

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4. {!LANG-8ccb38bd66b6e5fc011f6fa45668c4aa!}

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1{!LANG-2d1f7af56b5c6bc8cffa5ee771f46088!}

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3. Organization of practical work -

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1. Let the goal for testing the knowledge of the new material (questions p.32)

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