ABYSSIA

UNDER CONSTRUCTION

by Chris Wayan, 2004

for William Beebe and Otis Barton, first voyagers into the abyss

down to map and regional tours - How I Built Abyssia - (don't click yet) peoples of Abyssia - Abyssia's evolution - Gazetteer -
More worlds? Planetocopia!

INTRODUCTION

Abyssia is an illustration of just how much water Earth has, and what a miracle it is we have any land at all. The recipe for Abyssia is simple:

  1. Remove the world's oceans (store safely. You'll need it soon)
  2. Now mark the altitude of every point on Earth, and make every depth a height, and every height a depth. Our ocean trenches are now huge mountain ranges; our ranges, trenches. Rugged, isn't it? It's as if you'd turned Earth inside out like a glove...
  3. Now pour your stored seawater back into the new seabeds--the Eurasian Sea, the African Sea, the American Seas. But they'll fill up fast. You'll reach the old coastlines with water to spare. Lots to spare. Keep pouring. Soon you'll be refilling the seabeds, and wondering how much land there'll be. Soon you'll be adding "if any." Keep pouring! Don't hold any back.
  4. Look for land. Good luck. Most of our abyssal plains, which you'd think would form new continents, have become shallow seas; those that rise above water are low and broken. Only 12% of Earth's surface is land! That's all.
Are you starting to realize what a wet planet this is? And how lucky we are that continental rock is so light! We're living on rafts, and don't know it.

Earth, what a name! Don't make me laugh. Drenchia, Drownia, Uptoyournosia! That's what we live on.

Map of Abyssia, a world-building experiment.

THE BASICS

WHY ABYSSIA?

Oh, partly for fun--all the deepest, secretest parts of Earth are suddenly center stage, and all the geography you know is just an oceanographic footnote! Just a little bias-correction for all my land-animal readers (you know who you are).

It was partly a dare, too--my friend Dan saw a sister-planet I was building, Inversia, where up is down and down is up, and he noticed that to preserve the distinctive outlines of the continents, I'd put a lot less water over the inverted land. Dan asked "What if you put ALL our water back, so the only land is our deepest abysses?" It was an interesting challenge, and harder to calculate than I expected (and no, I couldn't run my handy-dandy super-accurate 3-D dataset of Earth with a minus sign to turn it inside out. Done by hand, folks--and that means a margin of error of at LEAST 100 meters! In fact I was off by a whole kilometer at first, setting the coastline near the six-kilometer mark. I even did a quick map of this world: call it Abyssia Six. Catastrophic! Islands dot the sea, but their total area's less than Australia--not much over 1% of the surface. Then I found I'd made a math error and the real contour was around 4900 m. Better, but still blue.) I thought we'd end up with fair-sized continents--basically, all the abyssal plains would become land. Wrong!

Abyssia's my way of highlighting a problem most planetologists don't talk of much. After centuries of highly visible Martian deserts, and decades of Venus-as-Hell propaganda, we tend to think space is dry and other worlds all have drought problems; wonderful Earth has the optimal amount of water for a biosphere. But it's quite possible to have too much water, and frankly, Earth does. 10-20% more water would have changed our geography profoundly; continents would erode into tall, narrow platforms only half as big. Or if our tectonics had been just a bit less active, the relief a bit lower, like Venus... well, if Venus had oceans even two-thirds as deep as Earth's, only 8-10% of the surface would be land! Earth is wet.

I don't go as far as Peter Ward Douglas in "Rare Earth", who claims planets with world-seas and little land won't develop complex life (my world-model Lyr is 95% sea but still sustains a complex land-civilization); but still, experiments like Abyssia show how dangerously close Earth came to lacking land entirely. Only ruggedness saved us: and it arose from very active tectonics, courtesy of the tidal drag of our huge moon. How common is that?

THE LESSONS OF ABYSSIA

In some ways, drier is safer. Even 1% of our water would be enough for very extensive seas, after all; for three examples of dry biospheres, see Serrana (8%), Mars Reborn (1.5%?), or Tharn (0.2%!). Sealife concentrates in the surface layers, and the rain that landlife needs evaporates off the surface, too. Our seas are unnecessarily deep--so deep they were almost fatal.

In short: as we look for life elsewhere, remember: Earth may be precious to us for sentimental reasons, but it's not unique--not even optimal. Just good enough--and yet we're proof that's all life needs. We don't need to look for other Earths; our search can be much broader than that.

Map of Abyssia, a world-building experiment. Click a feature to go there.
TOURS

The following route snakes around Abyssia, covering all major features (don't bother clicking, no pages yet)

the Lena Is. (brr!) Atlantis -- Sargassia and the Caribbean -- Nazca and Chilea -- Morningtonia -- Agassiz -- South Pacifica -- East Pacifica -- Hawaiian Sea -- Pacifica Desert -- Filipinia -- Vityaz Is -- Tasman Is. -- Diamantina Pen. -- Whartonia -- Chagosia -- Somalia -- Mascarenia -- Crozetia -- Weddellia -- Argenta -- Pernambuco -- Angolia -- Tristania -- Agulhas -- Natalia --

Abyssia's homepage - map - (don't click yet) peoples of Abyssia - (don't click yet) Abyssia's evolution - regional tours - (don't click yet) Gazetteer


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