
joined Yeltsin in plotting what to do with the re-
calcitrant legislature. Shumeiko returned to the
government on September 22, after Yeltsin’s order
to dissolve parliament. The next month, Yeltsin
named him Minister of Press and Information.
Shumeiko switched to the newly created Fed-
eration Council, becoming chair of that house in
January 1994, a post that also gave him a seat on
the Russian Security Council. He formed his own
political movement, Reforms—New Course, in De-
cember 1994. Shumeiko lost his seat in January
1996, when Yeltsin changed the basis of member-
ship in the Federation Council. Since then, Shumeiko
has unsuccessfully tried to return to a legislative
office. As of 2003 he was chairman of the petro-
leum company Evikhon.
See also: YELTSIN, BORIS NIKOLAYEVICH
A
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E. R
OBERTSON
SIBERIA
Often called the “Wild East,” beautiful but austere,
Siberia is one of the least populated places on earth.
Western Siberia is the world’s largest and flattest
plain, across which tributaries of the Ob and Irtysh
rivers wend their way north to the Arctic Ocean.
This orientation means that in spring the mouths
of the rivers are yet frozen while their upper reaches
thaw, creating the world’s largest peat bog in the
middle of the plain; thus, the lowland is arable only
in the extreme south. Eastern Siberia and the Rus-
sian Far East tend to be rugged and mountainous,
with thin soils at best. Beneath this chiefly soil-less
veneer lies some of the world’s oldest rock. Higher
mountains and active volcanoes rise along the east-
ernmost edge, where the Pacific Ocean plate subducts
beneath Asia. Here also the majority of the rivers
drain northward, perpendicular to the main east-
west axis of settlement. Only along the Pacific
seaboard do the rivers flow east, the longest of
which is the Amur, which, together with its trib-
utaries, forms the boundary between China and
Russia. On the border between Eastern Siberia and
the Russian Far East, the region boasts the world’s
oldest and deepest lake, Baikal. Including some of
the purest water on earth, Lake Baikal holds more
than twenty percent of the globe’s freshwater re-
sources.
Human settlement resembles a mostly urban,
beaded archipelago strung along the Trans-Siberian
Railroad from the Urals cities of Chelyabinsk and
Yekaterinburg to Vladivostok, 4,000 miles away in
the east. In between, rest the large cities of Novosi-
birsk, Krasnoyarsk, Irkutsk, and Khabarovsk.
Novosibirsk, which means “New Siberia,” is largest
of all with 1.5 million people.
The densest settlement pattern conforms to
Siberia’s least severe climates, which align them-
selves in parallel belts from harsh to harshest at
right angles to a southwest-northeast trend line.
Deep within the interior of Asia and surrounded by
mostly frozen seas, Siberia experiences the most
continental climates on the planet. One-time max-
ima of more than ninety degrees Fahrenheit (35 de-
grees Celsius) are possible in the relatively short
Siberian summers except along the coasts, whereas
one-time minima of minus-ninety degrees Fahren-
heit (–68 degrees Celsius) have been recorded in the
long winters of Sakha (Yakutia). This broad range
of temperatures is not recorded anywhere else. For-
tunately, the winter frost is typically dry and
windless, affording some relief to the isolated towns
and hamlets located in the sparsely populated
northeast.
Although western geographers accept the en-
tire northeastern quadrant of Eurasia as the region
known as Siberia, Russian geographers officially
accept only Western and Eastern Siberia as such,
excluding the Russian Far East, or Russia’s Pacific
Rim. Including the Russian Far East, Siberia spans
5,207,900 square miles (13,488,400 square kilo-
meters) and makes up more than three-fourths of
the Russian land mass. By this definition, Siberia is
a fourth bigger than Canada, the world’s second
largest country. It extends from the Ural Moun-
tains on the west to the Pacific Ocean on the east.
North to south it spans an empty realm from the
Arctic Ocean to the borders of Kazakhstan, Mon-
golia, and China. It is empty because, although it
occupies 23 percent of Eurasia, it environs less than
1 percent of the continent’s population. Siberia is
so massive that citizens of the U.S. state of Maine
are closer to Moscow than are residents of Siberia’s
Pacific Coast.
The Russian word Sibir has at least six contro-
versial origins, ranging from Hunnic to Mongolic
to Russian. The Mongol definition is “marshy for-
est,” which certainly typifies much of the Siberian
landscape.
To many Westerners, the name evokes a pop-
ular misconception that people who live in Siberia
are exiles or forced laborers. Although it is accurate
SIBERIA
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ENCYCLOPEDIA OF RUSSIAN HISTORY