World History Maps: The World vs PaleoEarth Uso & Estadísticas

World History Maps: The World, by World History Maps Inc, is a new and unique way of looking at history. Instead of an historical atlas which has maps showing the world (or a region) at a few significant years, or maps that try to compress decades or even centuries of change on to one map, we offer a different approach. Our interactive historical maps show the entire world for every single year in recorded history. This is an unprecedented amount of detail in time for the whole world that cannot be found anywhere else. The scalable maps allow even the smallest countries to be shown. Looking at History in this detail gives one a unique perspective. These are also the first historical maps to be made using GIS technology. Maps show countries of the world at the beginning of each year, with Major Tribes and Peoples. Maps are Scaleable and zoomable with popup information. Scrolling forward and backward is available with adjustable speeds. Maps can be pinned so you can toggle back and forth to compare different years. Following below are more details about how to use the apps.

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PaleoEarth

Earth is a dynamic planet. If anything has been constant throughout Earth history, it is its relentless state of flux -- from the ceaseless motion of tectonic plates to the ever-changing climate that eventually led to the birth of life itself to the steady bombardment of asteroids, some of which led to large-scale extinction events. PaleoEarth brings together a number of disparate data sets and provides a unique window into Earth's dynamic history. Key features include: * Shows the motion of continental plates, subduction zones (where oceanic crust sinks into the Earth's mantle) and mid-ocean ridges (where new oceanic crust is created) over the last 400 million years. * Shows sites of major asteroid impacts, tracing them from their original location at the time of impact to their current location, having been transported by the motion of tectonic plates. * Shows how Earth's temperature and atmospheric CO2 concentration compare to present-day values, over the last 400 million years. * Traces the borders of a given country back in time -- over the last 400 million years -- and shows how a number of large countries, e.g. the Russian Federation and the People's Republic of China have resulted from the agglomeration of smaller continental plates.