Thermohaline circulation estimates of the thermohaline circulation or, more accurately, the meridional overturning circulation. The deep water masses that participate in the MOC have chemical, temperature and isotopic ratio signatures and can be traced, their flow rate calculated, and their age determined. These include Pa / Th ratios. The Gulf Stream, together with its northern extension towards Europe, the North Atlantic Drift, is a powerful, warm, and swift Atlantic ocean current that originates at the tip of Florida, and follows the eastern coastlines of the United States and Newfoundland before crossing the Atlantic Ocean. The process of western intensification causes the Gulf
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.