Damn, so much to respond to, and I don't have regular www access this week, so I can't really write elaborated comments now...
Basilius wrote:OK. I think Cedh's datings for the Three Waves can be reconsidered *if that's really needed*. So let's consider "-20 KY", "-15 KY" etc. just conventional labels.
That "Theory" was really just an ad-hoc explanation, so the details can definitely be modified. I like Sal's elaboration; this should be unified into a wiki article.
Basilius wrote:For example, the shortest route I can imagine for an early migration to the Twin Continents is Lotoka coast - Thumapahìthì - Ttiruku - Zeluzhia - the peninsula protruding from "Antarctis" - Western Twin Continent; therefore, a lot depends on how early the sound between Ttiruku and Zeluzhia could be crossed (it looks too wide for rafts and dugouts, doesn't it?).
I think the first crossing to Zeluzhia would probably be made via that small island arc at the northeastern tip of Zeluzhia. There, the largest distance between individual islands may well be below 50km.
The eastern part of Zeluzhia and the northern part of "Antarctica" are geologically the same continent; the strait between them is fairly shallow and also full of islands. I think it would be very likely that a maritime culture would develop quickly once humans get there, and such a culture might easily explore the coasts of "Antarctica" and eventually cross over to the northwestern "Twin". Only the southeastern Twin and the large islands east of Tuysáfa ("Anatolionesia" as mentioned in the Erhadzy grammar) and north of the NW Twin (this is "Lesan") would remain uninhabited by, say, 1000 YP.
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With regard to the map, Salmoneus wrote:My first reaction is that every continent now looks bigger and more shapelessly blobby than it did before.
Second reaction: what the hell has happened to the northeastern islands, and WHY? They made sense before, didn't they? [Having the islands extend in a ridge from the mainland would make sense as an old plate boundary, which would explain why it's above land when the rest of the plate isn't]
Third reaction: isn't it a bit weird having that subcontinent all by itself on the corner of a plate? I'd make a small plate covering it and the ocean to the south-east (creating a nesia in the process).
Fourth reaction: wouldn't it be nice to have at least a couple of islands somewhere going vaguely near the arctic?
Re Second/Third:
I never even considered the northeastern islands being at a plate boundary, but now you mention it, it does make sense. Possibly more so than having Siixtaguna and NW Tuysáfa on the same plate, as it is now (with submerged continental crust between, this explains why the Ttirukan islands are so large).
Re Fourth:
Adding some islands north of the Siixtaguna subcontinent is possible and not a big deal. It's more difficult north of the Western sphere or north of Tuysáfa for tectonic reasons.
Re First and the following:
Corumayas wrote:What I think we really, really need is a scale.
Sal's comments prompted me to check this. It turns out that the shape of S Peilaš (at least) will definitely have to be revised yet again: Assuming that Akana is identical in size to Earth, that large "blob", which would mostly be covered by tropical forest (if the western part isn't too dry for that), is almost twice the size of South America. The mountain range on its NW coast is about the same length as the Andes, if the islands are included:
Also, I still don't like how the north coast of Peilaš looks on a globe, and "Antarctica" is not completely tectonically plausible either (shape does not line up with plate borders). I'll have to revise these as well. I don't want to revisit anything in the Xšali - Aiwa - Ttiruku - Tuysáfa - Zeluzhia region, though.
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Basilius wrote:Also, I know that the general rule demands that the toponyms of Fáralo origin be in the standard translitteration, but I would definitely prefer an Anglicized form (without eng etc.), e. g. Lashaffanong.
Actually, I'm strongly in favour if
not using Anglicized forms anywhere on the wiki. I don't even like the fact that Naidda uses <sh> for /S/. (Obviously, using Anglicized forms here or on IRC if diacritics are not available at that moment is OK, but I'd like to see the official Akana material free from such forms.) It follows from this that I would support using "Affanon" as the regular, native-based adjective, and to replace "Affanonic" either with the native name of the language or with another in-world designation. As a precedent: we've replaced all Anglicized adjectives in the context of Dāiadak culture with Adātaized forms in
-ran a while ago, e.g. *Lasomian > Lasomoran.