North Atlantic Current eastward and becomes much broader and more diffuse. It then splits into a colder northeastern branch and a warmer eastern branch. As the warmer branch turns southward, most of the subtropical component of the Gulf Stream is diverted southward, and as a consequence, the North Atlantic is mostly supplied by subpolar waters, including a contribution from the Labrador Current recirculated into the NAC at 45°N. West of Continental Europe, it splits into two major branches. One branch goes southeast, becoming the Canary Current as it passes northwest Africa and turns southwest. The other major branch continues north along the coast
Drift Creek Bridge Drift Creek Bridge The Drift Creek Bridge is a covered bridge in Lincoln County in the U.S. state of Oregon. Built in 1914, the structure originally carried Drift Creek County Road over Drift Creek. The creek flows into Siletz Bay of the Pacific Ocean south of Lincoln City. The original bridge, about from the ocean, once carried the main north–south route along the coast. Newer bridges later carried most of the north–south traffic and, after a concrete bridge bypassed the Drift Creek Bridge in the 1960s, Lincoln County preserved it as a pedestrian crossing and a monument to 19th-century pioneers.