Difference between revisions of "Lethe (region)"
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==History== | ==History== | ||
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| + | ===The first Lethians=== | ||
The Lethian Islands, as they are now known, emerged from the [[Wikipedia:Atlantic_Ocean|North Atlantic]] as the product of a series of undersea volcanic eruptions and tectonic shifts. The main island, '''Lethe''', formed a bridge between Continental [[Wikipedia:Europe|Europe]], including what became the [[Wikipedia:British_Isles|British and Irish Isles]], and the northern islands of [[Wikipedia:Iceland|Iceland]] and [[Wikipedia:Greenland|Greenland]], serving as a way-station for many animal species. From the days of the [[Wikipedia:Cambrian_explosion|Cambrian Explosion]], when the scalding submarine vents fed a wide variety of peculiar aquatic creatures to the amphibians, insects, reptiles, and eventually mammals of later eras, the Islands hosted many lifeforms until the [[Wikipedia:Ice_age|Ice Ages]] rendered them almost uninhabitable. | The Lethian Islands, as they are now known, emerged from the [[Wikipedia:Atlantic_Ocean|North Atlantic]] as the product of a series of undersea volcanic eruptions and tectonic shifts. The main island, '''Lethe''', formed a bridge between Continental [[Wikipedia:Europe|Europe]], including what became the [[Wikipedia:British_Isles|British and Irish Isles]], and the northern islands of [[Wikipedia:Iceland|Iceland]] and [[Wikipedia:Greenland|Greenland]], serving as a way-station for many animal species. From the days of the [[Wikipedia:Cambrian_explosion|Cambrian Explosion]], when the scalding submarine vents fed a wide variety of peculiar aquatic creatures to the amphibians, insects, reptiles, and eventually mammals of later eras, the Islands hosted many lifeforms until the [[Wikipedia:Ice_age|Ice Ages]] rendered them almost uninhabitable. | ||
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Beyond this brief information, garnered from animal bones and other material evidence in and around a few well-preserved sites and from ancient bodies found within [[Wikipedia:Peat|peat]] bogs, little is known about these first colonists. Whence these settlers came is still a matter of conjecture, although based on the existing fossil and material record, the Islands appear to have been concurrently colonised by both the [[Wikipedia:Thule_people|Thule people]] and Western [[Wikipedia:Eurasia|Eurasians]]. It is unknown how these early peoples interacted, but by at least [[Wikipedia:3rd_millennium_BC|2500 BC]] they had established a broadly similar material culture throughout the archipelago comprised of coastal settlements of sandstone built into and atop of [[Wikipedia:Midden|middens]], as well as some within existing hills, as at [[Wikipedia:Skara_Brae|Skara Brae]], evincing maritime linkages with what became northern [[Wikipedia:Scotland|Scotland]]. | Beyond this brief information, garnered from animal bones and other material evidence in and around a few well-preserved sites and from ancient bodies found within [[Wikipedia:Peat|peat]] bogs, little is known about these first colonists. Whence these settlers came is still a matter of conjecture, although based on the existing fossil and material record, the Islands appear to have been concurrently colonised by both the [[Wikipedia:Thule_people|Thule people]] and Western [[Wikipedia:Eurasia|Eurasians]]. It is unknown how these early peoples interacted, but by at least [[Wikipedia:3rd_millennium_BC|2500 BC]] they had established a broadly similar material culture throughout the archipelago comprised of coastal settlements of sandstone built into and atop of [[Wikipedia:Midden|middens]], as well as some within existing hills, as at [[Wikipedia:Skara_Brae|Skara Brae]], evincing maritime linkages with what became northern [[Wikipedia:Scotland|Scotland]]. | ||
| − | Unlike the dwellers at Skara Brae, the early | + | Unlike the dwellers at Skara Brae, the early inhabitants of the Islands did not abandon such dwellings until around [[Wikipedia:22nd century BC|2100 BC]] despite the steadily worsening climate. This reticence was likely due to the difficulty of harvesting timber from the sturdy oak and fir trees deep inland with their existing stone tools and the relative abundance of aquatic food sources, notably whales, seals, and kelp. |
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| + | ==Bronze Age== | ||
| + | Based upon the presence of [[Wikipedia:Stannary|stannaries]] and [[Wikipedia:Copper|copper]] [[Wikipedia:Mine|mines]] throughout what is now Lethe, the [[Wikipedia:Bronze_Age|Bronze Age]] arrived in the Islands about [[Wikipedia:1700 BC|1700 BC]], approximately three centuries after it had first appeared in what became the British and Irish Isles. | ||
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| + | Widespread deforestation marked the Lethian Bronze Age, as did the manufacture of sea-going vessels capable of trading with [[Wikipedia:Europe|Europe]], the development of [[Wikipedia:Broch|brochs]] or [[Wikipedia:Atlantic_roundhouse|Atlantic roundhouses]] — the techniques for building which were likely imported from the [[Wikipedia:Hebrides|Hebrides]] — and of [[Wikipedia:Crannog|crannogs]] in the southern lake lands. | ||
{{Isselmere-Nieland}} | {{Isselmere-Nieland}} | ||
[[Category:Regions]] | [[Category:Regions]] | ||
Revision as of 03:54, 11 October 2006
Lethe, or more correctly, the Lethian Islands, is an archipelago situated north-northwest of Ireland and south-southeast of Iceland. The Solquist Sea separates the region from Iceland, whilst the Tichonian, Lethian, or Eastern Irish Sea divides it from Ireland.
The island chain is home to five countries. Clockwise from the north, these are Azbinia, which spans the entire northern third, Hoblingland, occupying the eastern middle third, Isselmere-Nieland that dominates the southern third with shores on both of the main island's coasts, Gudrof to the very south, and Wingeria in the western middle third.
History
The first Lethians
The Lethian Islands, as they are now known, emerged from the North Atlantic as the product of a series of undersea volcanic eruptions and tectonic shifts. The main island, Lethe, formed a bridge between Continental Europe, including what became the British and Irish Isles, and the northern islands of Iceland and Greenland, serving as a way-station for many animal species. From the days of the Cambrian Explosion, when the scalding submarine vents fed a wide variety of peculiar aquatic creatures to the amphibians, insects, reptiles, and eventually mammals of later eras, the Islands hosted many lifeforms until the Ice Ages rendered them almost uninhabitable.
Hominids came late to the Islands, arriving in the middle of the 7th millennium BC by which time the ice had finally receded. These first settlers were modern, late-Mesolithic to early-Neolithic homo sapiens sapiens hunter-gatherers who relied upon harvesting kelp and seaweed, fishing, whaling, and seabirds as well as rudimentary agriculture for much of their diet.
Beyond this brief information, garnered from animal bones and other material evidence in and around a few well-preserved sites and from ancient bodies found within peat bogs, little is known about these first colonists. Whence these settlers came is still a matter of conjecture, although based on the existing fossil and material record, the Islands appear to have been concurrently colonised by both the Thule people and Western Eurasians. It is unknown how these early peoples interacted, but by at least 2500 BC they had established a broadly similar material culture throughout the archipelago comprised of coastal settlements of sandstone built into and atop of middens, as well as some within existing hills, as at Skara Brae, evincing maritime linkages with what became northern Scotland.
Unlike the dwellers at Skara Brae, the early inhabitants of the Islands did not abandon such dwellings until around 2100 BC despite the steadily worsening climate. This reticence was likely due to the difficulty of harvesting timber from the sturdy oak and fir trees deep inland with their existing stone tools and the relative abundance of aquatic food sources, notably whales, seals, and kelp.
Bronze Age
Based upon the presence of stannaries and copper mines throughout what is now Lethe, the Bronze Age arrived in the Islands about 1700 BC, approximately three centuries after it had first appeared in what became the British and Irish Isles.
Widespread deforestation marked the Lethian Bronze Age, as did the manufacture of sea-going vessels capable of trading with Europe, the development of brochs or Atlantic roundhouses — the techniques for building which were likely imported from the Hebrides — and of crannogs in the southern lake lands.
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