Earth’s Tectonic Plates

When the concept of seafloor spreading came along, scientists recognized that it was the mechanism to explain how continents could move around Earth’s surface. Scientific data and observation now allows us to merge the ideas of continental drift and seafloor spreading into the theory of plate tectonics.Seafloor and continents move around on Earth’s surface, but what is actually moving? What portion of the Earth makes up the “plates” in plate tectonics? This question was also answered because of technology developed during the Cold War. The plates are made up of the lithosphere. During the 1950s and early 1960s, scientists set up seismograph networks to see if enemy nations were testing atomic bombs. These seismographs also recorded all of the earthquakes around the planet. The seismic records could be used to locate an earthquake’s epicenter, the point on Earth’s surface directly above the place where the earthquake occurs. Earthquake epicenters outline these tectonic plates. Mid-ocean ridges, trenches, and large faults mark the edges of these plates along with where earthquakes occur.

Map of the tectonic plates. The Eurasian plate includes Europe and Asia. Its northern borders (both east and west) meet up with the North American Plate, whose southern border is just below Alaska in the west, but follows the coastline down, so the southern border in the East is much further south. The Filipino plate is below both the Eurasian and North American plate, running along the southern border of each. The Pacific Plate shares a border with the Filipino plate spans the Pacific Ocean along the southern border of the North American Plate. The Juan de Fuca and Cocos plates are small plates sandwiched between the Pacific and North American plates on the East border of the Pacific plate. The Caribbean plate includes just central America and a portion of the ocean to its east. The Nazca Plate is between the Pacific Plate’s eastern border and the west border of the South American Plate. Along the Southern border of the South American Plate is the Scotia plate. directly to the West of the South American Plate is the African Plate. The African plate is along the southern border of both the North American Plate and the Eurasian Plate. The Arabian and Indian Plates are both small and run beside the African Plate (Arabian to the west, and Indian to the west of the Arabian Plate) along the Southern border of the Eurasian Plate. The Australian plate fills the space between the African and Indian Plates and the Pacific Plate. All space south of these plates is covered by the Antarctic plate.

The lithosphere is divided into a dozen major and several minor plates. The plates’ edges can be drawn by connecting the dots that mark earthquakes’ epicenters. A single plate can be made of all oceanic lithosphere or all continental lithosphere, but nearly all plates are made of a combination of both. Movement of the plates over Earth’s surface is termed plate tectonics. Plates move at a rate of a few centimeters a year, about the same rate fingernails grow.

How Plates Move

If seafloor spreading drives the plates, what drives seafloor spreading? Picture two convection cells side-by-side in the mantle. Hot mantle from the two adjacent cells rises at the ridge axis, creating new ocean crust. The top limb of the convection cell moves horizontally away from the ridge crest, as does the new seafloor. The outer limbs of the convection cells plunge down into the deeper mantle, dragging oceanic crust as well. This takes place at the deep sea trenches. The material sinks to the core and moves horizontally. The material heats up and reaches the zone where it rises again.