Do you remember Gondwanaland? The landmass that was made up of
the three large landmasses we now know as Africa, South America, and
Australia. Why did these continents drift apart? Was it
because of a large meteor or was it Continental Drift? We may never
know the answer to these questions but what if we were able to calculate
the continental drift of any landmass? What if you were able to know
about a hige continental colission before it happened? Our team will
devise a program that will calculate the continental drift.
Continental Drift is the hypothetical tendency or ability that the
continents are drifting slowly away from each other. The first detailed
and comprehensive theory of continental drift was propsed in 1912 by
Alfred Wegener, a German Meteorologist. Wegener postulated that
throughout most of time there was only one continent. In 1937 Alexander
L. Du Toit, a South African Geologist, modified Wegener's hypothesis by
saying that there are two primordial continents.
Our team plans to write a program that will calculate continental
drift using current cooridates and rates. To do this, the current
position, speed, and direction will have to be mapped into a series of
vectors and then added to the user-inputed vector to accomplish
computerized continental drift. Although the math is quite a bit more
complicated since we have to do some spherical geometry but we can do
it.
Calculating continental drift will pose a challenging feat of
high school level programming. Continental drift may not be as
important to the world as the world stock market but sometime in the
distant future, it may come in handy.