China & Mongolia By Felix Belevan Angel Cabrera

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China & Mongolia

By Felix Belevan

Angel Cabrera

Physical Coordinates

China

◦ 35 00 N, 105 00 E

Mongolia

◦ 46 00 N, 105 00 E

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Days & Nights

China

time difference: UTC+8 (13 hours ahead of Washington,

DC during Standard Time)

note: despite its size, all of China falls within one time zone

Mongolia

time difference: UTC+8 (13 hours ahead of Washington,

DC during Standard Time)

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Locations in reference

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Rocks & Minerals

China

◦ coal, iron ore, petroleum, natural gas, tin, tungsten, antimony, manganese, molybdenum, vanadium, magnetite, aluminum,

◦ lead, zinc, uranium

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Rocks & Minerals

Mongolia

◦ oil, coal, copper, molybdenum, tungsten, phosphates, tin, nickel, zinc, fluorspar, gold, silver, iron

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Plate Tectonics of the Area

China

◦ the continent is a product of complex, long-term interaction between the Siberia,

Tarim, North China,

Yangtze, South China,

Indian and Pacific palaeoplates plus other relatively small plates or blocks.

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Plate Tectonics of the Area

China

◦ Along the converging margins of these plates, fold zones formed as a result of the plate collisions, whereas in the centers of the plates, basins and plains were developed because of stable tectonic settings and sedimentation

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Plate Tectonics of the Area

Mongolia

◦ here are hot springs as a result of shifting plate

Regional geology:

◦ The geology of Mongolia is complex

◦ geological maps reveal the variety and complexity of rock types and structures, with representatives of all geological ages from

Precambrian to Tertiary tectonics

◦ The rocks record successive episodes of terrane accretions and consequent deformation. These tectonic boundaries encompass

‘plates’: collections of smaller terranes which formed as continental fragments were successively plastered against, and welded together

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China’s Terrain

 mostly mountains high plateaus, deserts in west plains, deltas, and hills in east

High possibility of earthquakes

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Mongolia’s Terrain

Much of eastern Mongolia is occupied by a plain, and the lowest area is a southwestto-northeast trending depression that reaches from the Gobi Desert region in the south to the eastern frontier.

Mongolia has three major mountain ranges. The highest is the Altai Mountains, which stretch across the western and the southwestern regions of the country on a northwest-tosoutheast axis. The Khangai

Mountains, mountains also trending northwest to southeast, occupy much of central and north-central Mongolia. These are older, lower, and more eroded mountains, with many forests and alpine pastures. The

Khentii Mountains near the

Russian border to the northeast of Ulaanbaatar, are lower still.

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The Highs & Lows

China

lowest point: Turpan

Pendi -154 m

 .085 PSI

◦ highest point:

Mount Everest

8,850 m

 4.9 PSI

Mongolia

lowest point: Hoh

Nuur 518 m

 .286 PSI

◦ highest point:

Nayramadlin Orgil

(Huyten Orgil) 4,374 m

 2.43 PSI

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Carbon Dioxide Levels

China

◦ 2 nd in the world

◦ 5,010,170 in thousands of metric tons

◦ Percentage of total emissions in reference to world: 18.4 %

Mongolia

◦ 97nth in world

◦ 8,553 in thousands of metric tons

◦ Percentage of total emissions in reference to world:

Less than 0.1 %

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Carbon Dioxide Levels

City side

(China)

◦ more car emissions and factory fumes

◦ less plants to filter out the CO2

◦ more respiration

Country Side (Mongolia)

◦ more plants and trees which act as air filterers

◦ less cars, factories

◦ less respiration

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Wind Patterns in Area

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Wind Patterns in Area

The enormous expanse of Asia and its abundance of mountain barriers and inland depressions have resulted in great differences between regions in solar radiation, atmospheric circulation, precipitation, and climate as a whole.

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Humidity in Areas

China

◦ Hong Kong

 Humidity: 94%

◦ Beijing

 Humidity: 44%

◦ Shanghai

 Humidity:77%

Mongolia

◦ Choir

 Humidity:71%

◦ Ulan Bator

 Humidity:63%

◦ Altai

 Humidity:42%

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Climate Zones in China

The Nanling overlooks the part of China where a tropical climate permits two crops of rice to be grown each year.

Subtropical in the south to subarctic in the north.

Monsoon winds, caused by differences in the heatabsorbing capacity of the continent and the ocean, dominate the climate.

Alternating seasonal air-mass movements and accompanying winds are moist in summer and dry in winter

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Climate Zones in China

The advance and retreat of the monsoons account in large degree for the timing of the rainy season and the amount of rainfall throughout the country. Very humid.

Tremendous differences in latitude, longitude, and altitude give rise to sharp variations in precipitation and temperature within

China. Although most of the country lies in the temperate belt, its climatic patterns are complex thus

◦ China has both marine or continental climates.

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Climate Zones in Mongolia

Mongolia is high, cold, and dry. It has an extreme continental climate with long, cold winters and short summers, during which most precipitation falls.

Average temperatures over most of the country are below freezing from November through March and are about freezing in April and October.

Summer extremes reach as high as 38° C in the southern Gobi region and 33° C in Ulaanbaatar.

Most of Mongolia is covered by discontinuous permafrost

(grading to continuous at high altitudes)

Mongolia's weather is characterized by extreme variability and shortterm unpredictability in the summer, and the multiyear averages conceal wide variations in precipitation, dates of frosts, and occurrences of blizzards and spring dust storms.

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Climate Zones in Mongolia

Known as "the land of blue sky",

Mongolia is a remarkable sunny country enjoying 250 sunny days a year. Mongolia has warm summers and extremely cold winters. The country has the world's most typical continental climate with extreme diurnal and annual ranges of temperature.

Some of the most dramatic examples we see come from retreating glaciers in high mountains or melting polar ice sheets.

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Ocean Bordering

China

◦ Pacific Ocean

 Salinity varies by latitude.

 The water near the equator is less salty than that found in the mid-latitudes

 Poleward of the temperate latitudes salinity is low, because little evaporation of seawater takes place in these frigid areas.

Mongolia

◦ Landlocked

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Weather Disturbances

China

◦ frequent typhoons

◦ damaging floods

◦ Tsunamis

◦ earthquakes

◦ droughts

Mongolia

◦ dust storms

◦ grassland and forest fires

◦ harsh winter conditions

◦ earthquakes in the north and west

◦ Zud (extreme winter conditions)

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Biomes of Area

China

◦ Deciduous Forest

Biome

◦ temperate grassland

◦ Desert

◦ temperate forests

Mongolia

◦ Taiga (a subarctic, barren coniferous forest)

◦ Gobi (desert)

◦ Central Steppe (a dry grassy plain)

◦ Altai (mountains and valleys)

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China Population

China

◦ 1,330,044,605

◦ Post-productive

◦ Growth in area

0.629%

◦ Nation is trying to stabilize itself due to the high cost of living

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Mongolia Population

Mongolia

◦ 2,996,081

◦ Reproductive

◦ Growth in area

1.493%

◦ Nation is growing, and demanding more resources

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References

 http://findarticles.com/p/articles/ mi_qa3672/is_200501/ai_n9484

132 http://209.85.207.104/search?q= cache:Kh-

A6qrSA0UJ:nationalzoo.si.edu/A nimals/GiantPandas/PandaEducat ion/CurriculumGuides/9-

12/9to12BiomesAct2.pdf+biome

+of+china&hl=en&ct=clnk&cd=

5&gl=us https://www.cia.gov/library/publi cations/the-worldfactbook/geos/mg.html

https://www.cia.gov/library/publi cations/the-worldfactbook/geos/ch.html

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