Humanities › Geography How Many Continents Are There? Do you count five, six, or seven continents? Share Flipboard Email Print Buena Vista Images/Getty Images Geography Basics Physical Geography Political Geography Population Country Information Key Figures & Milestones Maps Urban Geography By Matt Rosenberg Geography Expert M.A., Geography, California State University - Northridge B.A., Geography, University of California - Davis Matt Rosenberg is an award-winning geographer and the author of "The Handy Geography Answer Book" and "The Geography Bee Complete Preparation Handbook." our editorial process Matt Rosenberg Updated August 18, 2019 A continent is typically defined as a very large landmass, surrounded on all sides (or nearly so) by water and containing a number of nation-states. However, when it comes to the number of continents on Earth, experts don't always agree. Depending on the criteria used, there may be five, six, or seven continents. Sounds confusing, right? Here's how it all sorts out. Defining a Continent The "Glossary of Geology," which is published by the American Geosciences Institute, defines a continent as “one of the Earth’s major landmasses, including both dry land and continental shelves." Other characteristics of a continent include: Areas of land that are elevated in relation to the surrounding ocean floorA variety of rock formations, including igneous, metamorphic, and sedimentary A crust that is thicker than those of the surrounding oceanic crusts. For example, the continental crust may vary in thickness from about 18 to 28 miles in depth, whereas oceanic crust is usually about 4 miles thickClearly-defined boundaries This last characteristic is the most controversial, according to the Geological Society of America, leading to confusion among experts as to how many continents there are. What's more, there is no global governing body that has established a consensus definition. How Many Continents Are There? If you went to school in the United States, chances are you were taught that there are seven continents: Africa, Antarctica, Asia, Australia, Europe, North America, and South America. But using the criteria defined above, many geologists say there are six continents: Africa, Antarctica, Australia, North and South America, and Eurasia. In many parts of Europe, students are taught that there are only six continents, and teachers count North and South America as one continent. Why the difference? From a geological perspective, Europe and Asia are one large landmass. Dividing them into two separate continents is more of a geopolitical consideration because Russia occupies so much of the Asian continent and historically has been politically isolated from the powers of Western Europe, such as Great Britain, Germany, and France. Recently, some geologists have begun arguing that room should be made for a "new" continent called Zealandia. This landmass lies off the eastern coast of Australia. New Zealand and a few minor islands are the only peaks above water; the remaining 94 percent is submerged beneath the Pacific Ocean. Other Ways to Count Landmasses Geographers divide the planet into regions for ease of study. The Official Listing of Countries by Region divides the world into eight regions: Asia, the Middle East and North Africa, Europe, North America, Central America and the Caribbean, South America, Africa, and Australia and Oceania. You can also divide the Earth's major landmasses into tectonic plates, which are large slabs of solid rock. These slabs consist of both continental and oceanic crusts and are separated by fault lines. There are 15 tectonic plates in total, seven of which are roughly ten million square miles or more in size. Not surprisingly, these roughly correspond to the shapes of the continents that lie atop them. Sources Mortimer, Nick. "Zealandia: Earth’s Hidden Continent." Volume 27 Issue 3, The Geological Society of America, Inc., March/April 2017.Neuendorf, Klaus K.E. "Glossary of Geology." James P. Mehl Jr., Julia A. Jackson, Hardcover, Fifth Edition (revised), American Geosciences Institute, November 21, 2011.