Abstract
We have used average continental elevations for 1‐degree‐square areas to construct detailed continental hypsographic curves. The curves available up to the present have been those prepared by Kossinna, but they suffer from some drawbacks, the most important being that the elevation interval is for the most part 1 km, which does not allow for very detailed work. Consequently, we have given data for each 0.1 km interval of elevation. The availability of the data on tapes allowed us also to make calculations of the average elevation of each continent, an important normalizing parameter when comparing continental hypsographic curves, and to add on the effects of the continental shelves. It has also allowed us to recalculate the amount of continent antipodal to continent and to produce a map of the world showing these areas. We have also used the detailed curves and the amounts of continental flooding during the Neozoic to derive records of sea level variation necessary to explain the amount of flooding for each continent through time.
Highlights
It has been over 60 years since data have been presented on continental hypsographic curves
Oceanic hypsography has been updated since Kossinna's papers by Menard and Smith [1966], and we felt that it was time for a new look at continental hypsography
By having more closely spaced contours it is possible to study anomalies in the hypsographic curve, such as that produced by the Tibetan plateau, which will be discussed below
Summary
It has been over 60 years since data have been presented on continental hypsographic curves. Kossirma [1921, 1933] has given the most recent information about continental hypsography. Oceanic hypsography has been updated since Kossinna's papers by Menard and Smith [1966], and we felt that it was time for a new look at continental. Kossinna's analysis presented data at 0.2, 0.5, or. One of our objectives was to present data at much more closely spaced intervals of elevation. By having more closely spaced contours it is possible to study anomalies in the hypsographic curve, such as that produced by the Tibetan plateau, which will be discussed below. We can improve the values for the average elevations of the continents, which are good normalizing factors when comparing continental hypsographic curves [Harrison et al, 1981]
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