The Physical Geography of Europe. Europe’s Latitude v. US.

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Presentation transcript:

The Physical Geography of Europe

Europe’s Latitude v. US

Satellite View of Europe

3,800 square miles

REGIONSREGIONSREGIONSREGIONS REGIONSREGIONSREGIONSREGIONS

Continents by Size (sq. km.) Asia44,579,000Africa30,065,000 North America 24,256,000 South America 17,819,000 Antarctica13,209,000 Europe Europe9,938,000 Oceania (incl. Australia) Oceania (incl. Australia) 7,687,000

 Europe share a common landmass called Eurasia  Europe has an unusually long, irregular coastline that touches a number of bodies of water.  Atlantic Ocean  Baltic Sea  North Sea  Mediterranean Sea  Black Sea

 Most of Europe lies within 300 miles of a seacoast.  This closeness to the sea has shaped the lifestyles of its peoples.  About 25% of the Netherlands lies below sea level.  Coastal dunes have not always been helped in keeping out North Sea waters, so the Dutch since the Middle Ages have built dikes. Large banks of earth and stone, to hold back water.  With the dikes for protection, they have reclaimed lands called polders, once were drained and kept dry by the use of windmills. Today, other power sources run pumps to remove seawater. Polders provide hundreds of thousands of acres for farming and settlement.

 Europe is a large peninsula made up of smaller peninsulas.  In the far north of Europe lies the scenic Scandinavian Peninsula.  During the last Ice Age, in a process known as glaciation, glaciers formed and spread over the peninsula.  They carved out long, narrow, steep-sided inlets called fjords on the Atlantic coastline.  Much of Norway and northern Sweden is mountainous, but in southern Sweden, lowlands slope gently to the Baltic Sea.  In both countries, and in Finland, Ice Age glaciers left behind thousands of sparkling lakes.  The peninsula of Jutland forms the mainland part of Denmark and extends into the North Sea toward Norway and Sweden.  Glaciers deposited sand and gravel on Jutland’s flat western side and carved fjords into the slightly higher coastline on the east.  Flat plains or low hills make up most of Jutland’s interior.

Norwegian Fjords Glaciers cut deep valleys in the ocean during the Ice Age. e Glaciers cut deep valleys in the ocean during the Ice Age.

Transylvania in the Carpathian Mountains e Home of Vlad Tepeš, the Drakul (“Count Dracula”)

Northern Peninsulas Jutland Peninsula Scandinavian Peninsula

 The Iberian Peninsula extends off the southern edge of Europe.  Home to Spain and Portugal, the peninsula separates the Atlantic Ocean from the Mediterranean Sea.  Only 20 miles of water at the Strait of Gibraltar separates the peninsula’s southern tip from Africa.  Most of the Iberian Peninsula is a semiarid plateau, rising above slender coastal plains.  To the north, the Pyrenees Mountains cut off the peninsula from the rest of Europe.  The people of the Iberian Peninsula until modern times were relatively isolated from the rest of Europe and were oriented toward the sea.  The Apennine Peninsula, where Italy is located, extends like a giant boot into the Mediterranean Sea.  Its long coastline varies from high, rocky cliffs to long, sandy beaches.  Forming the peninsula’s spine are the Apennines, a geologically young mountain chain that includes an active volcano – Mount Vesuvius, near the city of Naples.  In Southeastern Europe lies the Balkan Peninsula.  Bounded by the Adriatic and Ionian Seas on the west and the Aegean and Black Seas on the east, the Balkan Peninsula holds a tangle of mountain ranges and valleys that stretch southward from the Danube River.

Southern Peninsulas Iberian Peninsula Italian Peninsula Balkan Peninsula Anatolean Peninsula Crimean Peninsula

Mt. Vesuvius, Italy e 1944 eruption e Pompeii, 79 CE e Herculaneum, 79 CE

PeninsulasPeninsulasPeninsulasPeninsulas PeninsulasPeninsulasPeninsulasPeninsulas Scandinavian Pen. Jutland Pen. Iberian Pen. Italian Pen.Balkan Pen. Anatolean Pen. Crimean Pen. Peloponnesian Pen.

 Iceland is located south of the Arctic Circle in the North Atlantic Ocean.  Iceland has volcanoes, hot springs, and geysers.  Grassy lowlands stretch along Iceland’s coast, but the land rises sharply to form a large inland plateau.  The British Isles lie northwest of the European mainland.  They consist of two large islands, Great Britain and Ireland, and thousands of smaller islands.  Mountain ranges, plateaus, and deep valleys make up most of northern and western Great Britain, and low hills and gently rolling plains dominate the south.  Ireland is a lush green land of cool temperatures and abundant rainfall.  Other islands:  Sicily  Sardinia  Corsica  Crete  Cyprus

 Europe’s northwestern mountains have some of the earth’s most ancient rock formations.  Rounded by eons of erosion and glaciation, these ranges feature relatively low peaks, such as Ben Nevis, the highest mountain in the British Isles at 4,406 ft.  Extending from the Iberian Peninsula to eastern Europe, the central uplands consist of low, rounded mountains and high plateaus with scattered forests. This region includes the Meseta, Spain’s central plateau, and the Massif Central, France’s central highlands.  Southern Europe’s geologically younger mountains are high and jagged.  As the earth’s crust lifted and folded, the Pyrenees Mountains were thrust upward to more than 11,000 ft.  Created by glaciation and folding, the mountain system known as the Alps forms a crescent from southern France to the Balkan Peninsula. The highest peak is Mont Blanc at 15,771 feet.

The Alps e Cover most of Switzerland, Austria, and parts of Italy and France.

Mt. Blanc in the Alps e Highest mountain in the Alps: 15,771 feet

Transylvania in the Carpathian Mountains e Home of Vlad Tepeš, the Drakul (“Count Dracula”)

 Europe’s broad plains curve around the highlands.  The North European Plain stretches from southeastern England and western France eastward to Poland, Ukraine, and Russia.  The plain’s fertile soil and wealth of rivers originally drew farmers to the area, and the plain is still a major agricultural region.  The southern edge is especially fertile because deposits of loess, a fine, rich, wind-borne soil, cover it.  Deposit of coal, iron ore, and other minerals found on the North European Plain led to western Europe’s industrial development during the 1800s.  Today many of Europe’s largest cities, such as Paris and Berlin, are located on the plain.  Great Hungarian Plain, extends from Hungary to Croatia, Serbia, and Romania.

 The Rhine is the most important river in western Europe.  It flows from the Swiss Alps through France and Germany and into the Netherlands, connecting many industrial cities to the busy port of Rotterdam on the North Sea.  The Danube, which flows from Germany’s Black Forest to the Black Sea, is eastern Europe’s major waterway.  Each year ships and barges carry millions of tons of cargo on the Danube.  In 1992 the Main River, a tributary of the Rhine, became connected to the Danube when the Main-Danube Canal was completed.

RESOURCESRESOURCESRESOURCESRESOURCES RESOURCESRESOURCESRESOURCESRESOURCES

Major Industrial Resources

Oil Export Routes in the Caucasus Area