|
 Holesov, Czech Republic
Karlovy Vary, Czech Republic
Ostrava / Mosnov, Czech Republic
Praha / Ruzyne, Czech Republic
Brno / Turany, Czech Republic
Location: Central Europe, southeast of Germany
Geographic coordinates: 49 45 N, 15 30 E
Map references: Europe
Area:
total: 78,866 sq km
land: 77,276 sq km
water: 1,590 sq km
Area - comparative: slightly smaller than South Carolina
Land boundaries:
total: 1,881 km
border countries: Austria 362 km, Germany 646 km, Poland
658 km, Slovakia 215 km
Coastline: 0 km (landlocked)
Maritime claims: none (landlocked)
Climate: temperate; cool summers; cold, cloudy, humid winters
Terrain: Bohemia in the west consists of rolling plains,
hills, and plateaus surrounded by low mountains; Moravia in the
east consists of very hilly country
Elevation extremes:
lowest point: Elbe River 115 m
highest point: Snezka 1,602 m
Natural resources: hard coal, soft coal, kaolin, clay, graphite,
timber
Land use:
arable land: 41%
permanent crops: 2%
permanent pastures: 11%
forests and woodland: 34%
other: 12% (1993 est.)
Irrigated land: 240 sq km (1993 est.)
Natural hazards: flooding
Environment - current issues: air and water pollution in
areas of northwest Bohemia and in northern Moravia around Ostrava
present health risks; acid rain damaging forests
Environment - international agreements:
party to: Air Pollution, Air Pollution-Nitrogen Oxides, Air
Pollution-Sulphur 85, Air Pollution-Sulphur 94, Air Pollution-Volatile
Organic Compounds, Antarctic Treaty, Biodiversity, Climate Change,
Endangered Species, Environmental Modification, Hazardous Wastes,
Law of the Sea, Nuclear Test Ban, Ozone Layer Protection, Ship Pollution,
Wetlands
signed, but not ratified: Air Pollution-Persistent Organic
Pollutants, Antarctic-Environmental Protocol, Climate Change-Kyoto
Protocol
Geography - note: landlocked; strategically located astride
some of oldest and most significant land routes in Europe; Moravian
Gate is a traditional military corridor between the North European
Plain and the Danube in central Europe
Geography
The Czech Republic is situated approximately in the geographical
center of Europe and has an area of 78,866 sq. km. It is a landlocked
country 326 km from the Baltic and 322 km from the Adriatic. It
shares borders with Germany (810 km), Poland (762 km), Austria (466
km) and Slovakia (265 km).
The highest point of elevation is the peak of Mt. Snezka (1,602
m above sea level) and the lowest point of elevation is near Hoensko
where the River Labe leaves Czech territory (117 m above sea level).
Climate
The Czech Republic has a humid, continental climate, with cold winters
and warm summers. The average temperature range in Prague is -5.3°
C (22.5° F) to -0.4° C (32.7° F) in January and 11.8° C (53.2° F)
to 23.3° C (73.9° F) in July.
Temperatures generally decrease with increasing altitude. Prague
receives an average of about 410 mm (about 16 in) of precipitation
annually. Precipitation is generally heaviest during the summer
months.
Background: After World War II, Czechoslovakia fell within
the Soviet sphere of influence. In 1968, an invasion by Warsaw Pact
troops ended the efforts of the country's leaders to liberalize
party rule and create "socialism with a human face."
Anti-Soviet demonstrations the following year ushered in a period
of harsh repression. With the collapse of Soviet authority in 1989,
Czechoslovakia regained its freedom through a peaceful "Velvet Revolution."
On 1 January 1993, the country underwent a "velvet divorce" into
its two national components, the Czech Republic and Slovakia. Now
a member of NATO, the Czech Republic has moved toward integration
in world markets, a development that poses both opportunities and
risks.
FORMER CZECHOSLOVAKIA
Czechoslovakia
GEOGRAPHY
Size: Approximately 127,905 square kilometers.
Topography: Generally irregular terrain. Western
area, including natural basin centered on Prague, part of north-central
European uplands. Eastern region made up of northern reaches of
Carpathian Mountains and Danube Basin lands.
Climate: Predominantly continental but varies
from moderate temperatures of Western Europe to more severe weather
systems affecting Eastern Europe and the western Soviet Union.
SOCIETY
Population: Estimated at 15.6 million in July
1987. Population growth rate 0.3 percent in 1987.
Education and Literacy: Education free at all
levels and compulsory from age six to sixteen. Vast majority of
population literate. Highly developed system of apprenticeship training
and vocational schools supplements general secondary schools and
institutions of higher education.
Health: Free health care available to all citizens.
National health planning emphasizes preventive medicine; factory
and local health-care centers supplement hospitals and other inpatient
institutions. Substantial improvement in rural health care in 1960s
and 1970s.
Language: Czech and Slovak recognized as official
languages; they are mutually intelligible.
Ethnic Groups: In 1987 Czechs represented roughly
63 percent of population and Slovaks 31 percent. Hungarians, Ukrainians,
Poles, Germans, and Gypsies principal minority groups.
Religion: Religious freedom constitutionally guaranteed
but limited in practice. Major religious organizations operate under
government restrictions. Reliable information on religious affiliation
during post-World War II era lacking, but principal denominations
Roman Catholic Church, Czechoslovak National Church, Slovak Evangelical
Church, Evangelical Church of Czech Brethren, and Uniate Church.
Data as of August 1987
Czechoslovakia
GEOGRAPHY AND ENVIRONMENT
Topography and Drainage
The country's 127,905 square kilometers divide topographically
as well as historically into three major areas: Bohemia, Moravia,
and Slovakia, Bohemia consists of the five western political divisions,
or kraje (sing., kraj): Zapadocesky (West Bohemia),
Severocesky (North Bohenia), Jihocesky (South Bohenia), Vychodocesky
(East Bohenia), and Stredocesky (Central Bohenia). Moravia consists
of the two central political divisions: Severomoravsky (North Moravia)
and Jihomoravsky (South Moravia). Slovakia consists of the three
eastern political divisions: Zapadoslovensky (West Slovakia), Stredoslovensky
(Central Slovakia), and Vychodoslovensky (East Slovakia). The three
Slovak kraje constitute the Slovak Socialist Republic;
the other seven kraje constitute the Czech Socialist Republic.
Kraje are further subdivided into okresy (sing.,
okres), roughly equivalent to countries in the United States.
The areas of western Bohemia and eastern Slovakia belong to different
mountain and drainage systems. All but a minute fraction of the
Bohemian region drains into the North Sea by way of the Vltava (Moldau)
and Labe (Elbe) rivers. The hills and low mountains that encircle
this area are part of the north-central European uplands that extend
from southern Belgium, through the central German lands, and into
Moravia. These uplands, which are distinct from the Alps to the
south and the Carpathian Mountains to the east, are known geologically
as the Hercynian Massif. Most of Slovakia drains into the Danube
(Dunaj) River, and its mountains are part of the Carpathians, which
continue eastward and southward into Romania.
The uplands of Moravia are a transition between the Hercynian Massif
and the Carpathians and are in contrast with them by having more
nearly north-south ridge lines. Most of Moravia drains southward
to the Danube, but the Odra (Oder) River rises in the northeast
and drains a sizable portion of the northern region .
Data as of August 1987
Czechoslovakia
Bohemia
Bohemia's topography has fostered local solidarity and a common
set of economic interests. The area is ringed with low mountains
or high hills that effectively serve as a watershed along most of
its periphery (although they do not lie along the border to the
south and southeast). Streams flow from all directions through the
Bohemian Basin toward Prague (Praha).
In the northwest, the Krusne Hory (Ore Mountains) border on the
German Democratic Republic (East Germany) and are known to the Germans
as the Erzgebirge; the Sudeten Mountains in the northeast border
on Poland in an area that was part of Germany before World War II.
The Cesky Les, bordering on the Federal Republic of Germany (West
Germany), and the Sumava Mountains, bordering on West Germany and
Austria, are mountain ranges that form the western and southwestern
portions of the ring around the Bohemian Basin. Both are approximately
as high as the Krusne Hory. Bohemia's mountainous areas differ greatly
in population. The northern regions are densely populated, whereas
the less hospitable Cesky Les and Sumava Mountains are among the
most sparsely populated areas in the country.
The central lands of the Bohenian Basin are lower in elevation,
but their features vary widely. There are small lakes in the central
southern region and in the Vltava Basin north of Prague. Some of
the western grain lands are gently rolling, while other places have
deep gorges cut by streams (such as the Vltava River). A large area
southwest of Prague has a broken relief pattern that is typical
of several other areas.
Data as of August 1987
Czechoslovakia
Moravia
Moravia is a topographic borderland situated between Bohemia and
Slovakia. Its southwest-to-northeast ridge lines and lower elevations
made it useful as a route for communications and commerce from Vienna
to the north and northeast during the period of Austrian domination
of Central Europe.
The central and southern Moravian lowlands are part of the Danube
Basin and are similar to the lowlands they adjoin in southern Slovakia.
The upland areas are smaller and more broken than those of Bohemia
and Slovakia. The northwest hills are soft sandstone and are cut
by deep gorges. South of them, but north of Brno, is a karst limestone
area with underground streams and caves. These and the other uplands
west of the Morava River are associated with the Hercynian Massif.
The land to the east of the Morava is called Carpathian Moravia.
Data as of August 1987
Czechoslovakia
Slovakia
Slovakia's landforms do not make it as distinctive a geographic
unit as Bohemia. Its mountain ranges generally run east-west and
tend to segregate groups of people; population clusters are most
dense in river valleys. The highest elevations are rugged, have
the most severe weather, and are the most sparsely settled. Some
of the flatlands in southwestern Slovakia are poorly drained and
support only a few people. The main mountain ranges are the Vysoke
Tatry (High Tatras) and the Slovenske Rudohorie (Slovak Ore Mountains),
both of which are part of the Carpathians. The Vysoke Tatry extend
in a narrow ridge along the Polish border and are attractive as
both a summer and a winter resort area. The highest peak in the
country, Gerlachovsky Stit (also known as Gerlachovka), with an
elevation of about 2,655 meters, is in this ridge. Snow persists
at the higher elevations well into the summer months and all year
long in some sheltered pockets. The tree line is at about 1,500
meters. An ice cap extended into this area during glacial times,
leaving pockets that became mountain lakes.
The Slovak lowlands in the south and southeast, bordering on Hungary,
are part of the greater Danube Basin. From a point slightly south
of the Slovak capital of Bratislava, the main channel of the Danube
River demarcates the border between Czechoslovakia and Hungary for
about 175 kilometers. As it leaves Bratislava, the Danube divides
into two channels: the main channel is the Danube proper, and the
northern channel is the Little Danube (Maly Dunaj). The Little Danube
flows eastward into the Vah River, which converges with the main
Danube at Komarno. The land between the Little Danube and the Danube
is known as the Vel'ky Zitny Ostrov (Great Rye Island), a marshland
maintained for centuries as a hunting preserve for the nobility.
Dikes and artificial drainage have made it possible to cultivate
the land for grain production, but it is still sparsely settled.
Data as of August 1987
Czechoslovakia
Climate
Czechoslovakia's central European location influences its climate.
Although the continental weather systems that dominate Eastern Europe
prevail throughout the country, western regions are frequently influenced
by the maritime weather prevalent in Western Europe. When the systems
to the north are weak, Mediterranean weather may occasionally brush
southern parts of the country.
Winters are fairly cold, cloudy, and humid, although high humidity
and cloud cover tend to be more prevalent in valleys and lower areas.
Light rain or snow is frequent. The mountains are covered with snow
from early November through April, and accumulations are deep in
some places. Lower elevations rarely have more than fifteen centimeters
of snow cover at a time.
Summers are usually pleasant. There is heavy rainfall, but it comes
in sporadic showers, making for many warm, dry days with scattered
cumulus clouds. Prevailing winds are westerly; they are usually
light in summer (except during thunderstorms) and somewhat stronger
in winter.
Average temperatures in Prague, which is representative of lowland
cities in Bohemia and Moravia, range between about 1°C in January
and about 19°C in July. Winters are chilly; summers have warm
afternoons and cool evenings. In the eastern parts of the country,
the temperature extremes are greater. Higher elevations, especially
those with western exposures, usually have a narrower temperature
range but on the average are considerably cooler. December, January,
and February are the coldest months; June, July, and August are
the warmest. Spring tends to start late, and autumn may come abruptly
in middle or late September. At lower elevations, frosts are rare
between the end of April and the beginning of October.
Rainfall varies widely between the plains and the upland areas.
Parts of western Bohemia receive only forty centimeters of rainfall
per year; some areas in the Vysoke Tatry average two meters. The
average rainfall in the vicinity of Prague is fortyeight centimeters.
Precipitation varies more than in other areas of Europe, which are
often dominated by maritime weather systems; consequently, droughts
and floods sometimes occur.
Despite the greater frequency of precipitation during the winter,
more than twice as much precipitation, or about 38 percent, falls
in the summer. The spring and autumn figures are about equal.
Data as of August 1987
|
