The 45th parallel north is an imaginary line of latitude circling the Earth, running exactly 45 degrees north of the equator. Parallels of latitude are horizontal lines used in cartography to specify north-south positions, with the equator being 0 degrees and the poles 90 degrees. This line is often cited as the geometrical halfway point between the equator and the North Pole. Its location marks a transition zone that influences climate, history, and physical geography across three continents.
Understanding the 45th Parallel North
The 45th parallel north is designated by its angular distance from the equator. While 45 degrees suggests the exact midpoint between the equator and the North Pole, the Earth’s shape introduces a slight variation. Because the planet is an oblate spheroid, bulging slightly at the equator, the actual halfway point is technically located about 10 miles (16 kilometers) farther north, near 45 degrees, 8 minutes, and 40 seconds north latitude.
The line is nearly symmetrical to the 45th parallel south, which circles the globe in the Southern Hemisphere. However, the northern line is the one most frequently referenced in geography and history because it crosses significantly more landmasses and population centers.
The Global Path of the Line
The 45th parallel north crosses a vast and diverse range of landscapes, spanning Europe, Asia, North America, and three major oceans.
In North America, the line makes landfall on the Pacific coast in Oregon and continues eastward. It bisects several U.S. states, including Idaho, South Dakota, Minnesota, and Wisconsin, and defines much of the border between Montana and Wyoming. It also runs through the Great Lakes region, crossing parts of Michigan and the Canadian provinces of Ontario and Quebec.
The parallel continues across the Atlantic and enters Europe, passing through France, traversing regions like the Aquitaine and RhĂ´ne-Alpes. It then clips northern Italy, running near cities like Turin and Voghera in Piedmont and Lombardy. Further east, the line crosses the Balkans, including parts of Croatia, Bosnia and Herzegovina, and the Serbian province of Vojvodina.
Entering Asia, the line crosses the northern Black and Caspian Seas, moving into the Russian Federation through the Caucasus region and Stavropol Krai. It then bisects Central Asia, passing through Kazakhstan and Mongolia. The 45th parallel eventually reaches the Pacific coast, crossing northeastern China and the northern tip of Hokkaido, Japan, before disappearing into the North Pacific Ocean.
Climate and Historical Importance
The 45th parallel north is positioned in the middle of the North Temperate Zone, which generally results in moderate climates characterized by four distinct seasons. This latitude features warm summers and cool to cold winters, though local climates vary considerably due to proximity to oceans and major currents. For instance, west coasts along the line, such as in Oregon and France, experience milder, wetter climates due to oceanic influence, while continental interiors see greater temperature extremes.
The favorable climate has made regions along or near the 45th parallel highly productive agricultural areas, especially for viticulture. Many renowned wine-producing areas in France and Italy are situated close to this line, benefiting from the balance of temperature and sunlight exposure.
Historically, the line has served as a reference point for political demarcation. In North America, the 45th parallel was used to define sections of the border between the United States and Canada, particularly between Quebec and New York and Vermont. This boundary, sometimes called the Collins–Valentine line, was established after the Seven Years’ War. Subsequent surveys showed the actual monuments were placed slightly north of the true 45th degree. Its clear geometric position made it a convenient choice for establishing early political boundaries.