As spring arrives, the Northern Hemisphere gains daylight at different rates. See how much your region benefits from the seasonal shift with a NOAA-based map showing daylight changes across the U.S.
Read more: How Much Daylight Is Gained in the U.S. Between the Spring Equinox and Summer Solstice?
Dive into the captivating shifts of Earth’s North Magnetic Pole over centuries, uncovering its implications for navigation, the science behind geomagnetic reversals, and the evolving strength of our planet’s magnetic field.
Read more: Tracing the Dance of Earth’s Magnetic North: A Journey Through Time
The Total Surface Area of our planet is about 509.6 million km² or 197 million mi². The land occupies only 29% of the Earth’s Surface (148.3 million km2 or 57.3 million mi²). The largest countries by surface area are Russia (3.35%), Canada (1.96%), China (1.88%), United States (1.87%), Brazil (1.67%), and Australia (1.51%). Together they occupy approximately 12.24% of the planet’s surface. 70% of the Earth’s total surface is covered with water (361. 7 million km² or 139. 7 million mi²).
Read more: Earth’s surface visualized
The face of our planet is shifting continuously by geological processes. Splitting supercontinent Pangaea, these tectonic plates have arranged the planet’s surface into 7 continent landmasses and 5 oceans. Here is a visualization of the significant events on planet Earth through its four billion year history.
Read more: The History Of The Earth From Formation To Present Day
Frans Blok has created a detailed inverse map of the world, where the deepest spots in the ocean become the highest mountains and the highest mountains become the deepest part of the ocean.
Read more: Inverted world mapPangea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras. It assembled from earlier continental units approximately 335 million years ago, fully assembled about 270 million years ago, and it began to break apart about 175 million years ago. In contrast to the present Earth and its distribution of continental mass, much of Pangea was in the southern hemisphere and surrounded by a super ocean, Panthalassa. Pangea was the most recent supercontinent to have existed and the first to be reconstructed by geologists.
Read more: Interactive Pangea map with international borders
The breakup of Pangaea, a supercontinent that existed around 335 million years ago, is a significant event in Earth’s geological history. Pangaea began to break apart during the Mesozoic Era, forming the continents as we recognize them today. The process of breakup and continental drift occurred due to the movement of tectonic plates beneath the Earth’s surface.
Read more: The breakup of PangaeaResearchers are revealing in a recent three-dimensional map of the Earth’s lithospheric magnetic field, created using data from a trio
Read more: New 3D map offers clues about anomalies in Earth’s magnetic field
World population density represented as elevation. Source: cartoma-hamelberg.com
Read more: Earth according to population densityA new version of the global vertical gravity gradient (map, recently published in the journal ‘Science’, shows unprecedented detail, helping
Read more: Global vertical gravity gradient visualisationThe point Nemo is the most remote place on the planet.
Read more: How far away can you get from everybody else?