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This is “Europe”, chapter 2 from the book Regional Geography of the World: Globalization, People, and Places (index.html) (v. 1.0). This book is licensed under a Creative Commons by-nc-sa 3.0 (http://creativecommons.org/licenses/by-nc-sa/ 3.0/) license. See the license for more details, but that basically means you can share this book as long as you credit the author (but see below), don't make money from it, and do make it available to everyone else under the same terms. This content was accessible as of December 29, 2012, and it was downloaded then by Andy Schmitz (http://lardbucket.org) in an effort to preserve the availability of this book. Normally, the author and publisher would be credited here. However, the publisher has asked for the customary Creative Commons attribution to the original publisher, authors, title, and book URI to be removed. Additionally, per the publisher's request, their name has been removed in some passages. More information is available on this project's attribution page (http://2012books.lardbucket.org/attribution.html?utm_source=header). For more information on the source of this book, or why it is available for free, please see the project's home page (http://2012books.lardbucket.org/). You can browse or download additional books there. i Chapter 2 Europe Identifying the Boundaries Europe is a continent of peninsulas, islands, and varied landforms. The traditional boundaries of the European continent include the North Atlantic Ocean to the west and Russia up to the Ural Mountains to the east. Since the Soviet Union’s collapse in 1991, Russia has been given its own identification and, in this text, is not included in the study of Europe. Russia will be discussed in Chapter 3. Greenland is located next to the North American country of Canada but has traditionally been considered a part of Europe because of Denmark’s colonial acquisition of the island. Greenland is physically more a part of North America. The Arctic Ocean creates a natural boundary to the north. The southern boundary of Europe is the Mediterranean Sea and includes the islands of Malta and Cyprus as independent countries. A portion of Turkey is in Europe, but Turkey is considered a part of Asia Minor and is usually included in the study of the Middle East region. The waterway in Turkey between the Black Sea and the Aegean Sea is the Bosporus, or the Istanbul Strait, which creates a natural border between Asia and Europe. Europe is also close to North Africa, and Morocco’s coast can be seen across the Strait of Gibraltar from Spain. 75 Chapter 2 Europe 2.1 Introducing the Realm LEARNING OBJECTIVES 1. Describe the various climate types and physical landforms of the European continent. 2. Explain how Europe’s physical geography has supported its development. 3. List Europe’s various natural resources. 4. Summarize the environmental concerns Europe faces. From the Roman Empire to the European Union (EU), Europe’s historical pattern of development is a model study in regional geography. From historic empires to diverse nation-states to a multicountry union, the continent struggles to confront the cultural forces that unite and divide it. The powerful impact European colonialism has had on the world since the Industrial Revolution is still felt today. The rural-to-urban shift prompted by the Industrial Revolution first impacted Europe and continues to impact developing countries. Understanding the geographic region of Europe is essential to understanding our world. This short summary of the basic concepts will provide a valuable lesson in globalization, which affects every human being on the planet. The concepts and principles that apply to Europe can also apply to other countries and regions. 76 Chapter 2 Europe Figure 2.1 Map of Europe Source: Map courtesy of University of Texas Libraries, http://www.lib.utexas.edu/maps/europe/txu- oclc-247233313-europe_pol_2008.jpg. Location and Climate Europe is a northern continent. All the British Isles, for example, fall above the fiftieth parallel. If we compare Europe’s position on a globe with that of the contiguous United States, we see that much of Europe lies north of the United States. Paris, France, is at about the same latitude as Fargo, North Dakota. Athens, Greece, is at about the same latitude as St. Louis, Missouri. Europe’s northern position affects its growing seasons and people’s moods, and it should be taken into consideration as an important influence in the evolution of the European character. Europe is also surrounded by bodies of water: the Atlantic Ocean borders Europe on the west, the Arctic Ocean borders Europe to the north, and many seas surround the various peninsulas and coastal regions. The oceans exert significant influence on the world’s climates. The oceans collect and store vast amounts of solar energy, particularly around the equator, and 2.1 Introducing the Realm 77 Chapter 2 Europe transport that heat with their currents. Ocean currents can move water for thousands of miles from one temperature zone to another. Because oceans can absorb so much heat, maritime climates are often milder than continental ones, with smaller temperature variations from day to night as well as from winter to summer. This influences not only temperature but also precipitation patterns over wide regions of Europe and the rest of the world. Water moderates coast environments in a number of ways. Water heats and cools more slowly than land. This heat inertia allows coastal communities to have climates that tend to be more moderate than one might imagine for places so far north. Interior Europe does not benefit from coastal waters and can have winters as cold as those found within the upper midwestern United States. Figure 2.2 The Dominant Climate Types of Europe The Gulf Stream1 is perhaps the most important current for Western Europe’s climate and is responsible for producing a temperate climate for a northern latitude location. Most of Western Europe has a moderate type C climate. The Gulf Stream 1. Ocean current that carries warmer water from the South originates in the Gulf of Mexico, where the waters are warmed. This powerful Atlantic to the North Atlantic current follows the Eastern Seaboard of the United States before crossing the and moderates the Atlantic Ocean for Europe. The Gulf Stream’s most dramatic effect can be found in temperature of Western Europe. the western coastal islands of Scotland, which has a mild enough climate to support 2.1 Introducing the Realm 78 Chapter 2 Europe some forms of tropical flora, even though it is a degree of latitude as far north as Hudson Bay, Canada. The coast of Norway provides another example. While most of Norway’s coastal area lies within the Arctic region, it remains free of ice and snow throughout the winter. People living farther inland and closer to Eastern Europe and Russia encounter the colder type D climates. Colder air sweeps down from the Arctic north or from eastern Siberia and provides colder winters in this eastern region. The Mediterranean Sea moderates the temperature to the south, providing a type C climate around its shores. Type C climates meet up with type E climates at or near the Arctic Circle in Norway and in Iceland. Four Main European Landforms Europe has four main landforms, many islands and peninsulas, and various climate types. The four main landforms include the Alpine region, Central Uplands, Northern Lowlands, and Western Highlands. Each represents a different physical part of Europe. The wide-ranging physical environment has provided Europe with an abundance of biodiversity. Biodiversity refers to diversity of the number of species in an ecosystem and the quantity of members in each species. The physical environment also provides natural resources and raw materials for human activities. Europe’s moderate climates and favorable relative location are supported by its access to the many rivers and seas. These advantageous developmental factors supported the development of the Industrial Revolution in Europe, which gave rise to highly technical and urban societies. Europe has emerged as one of the core economic centers of the global economy. Associated with the urbanization of Europe are high human population densities that have placed a strain on the natural environment. As result, there has been significant deforestation and the loss of natural habitat, which has in turn has decreased the realm’s level of biodiversity. Rivers are abundant in Europe and have provided adequate transportation for travel and trade throughout its history. Most of Europe is accessible by water transport either via the many rivers or along the extensive coastlines of the peninsulas and islands. Two main rivers divide Europe: the Danube and the Rhine. Both have their origins in the region of southern Germany on or near the border with Switzerland. The Rhine River flows north and empties into the North Sea in Rotterdam, Holland, one of the world’s busiest ports. The Danube flows east through various major European cities, such as Vienna, Budapest, and Belgrade before emptying into the Black Sea. 2.1 Introducing the Realm 79 Chapter 2 Europe Figure 2.3 Four Main Landforms of Europe: Western Highlands, Northern Lowlands, Central Uplands, and the Alpine Region Alpine Region The High Alps, which range from eastern France to Slovenia, are central to the Alpine region. Included in the Alpine Range are the Pyrenees, located on the border between France and Spain; the Apennines, running the length of Italy; the Carpathians, looping around Romania from Slovakia; and finally, the shorter Dinaric Alps in former Yugoslavia. Mountains usually provide minerals and ores that were placed there when the earth’s internal processes created the mountains.

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