This article belongs to the lore of Planet Gentu.

Vetuslithic Age

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Human Migration.png
Proposed map of the Great Migration, according to artifacts found in certain regions (its accuracy is disputed).
PeriodPrehistorical Era
Dates2.5 mya-10,000 BCE
Preceded bySeptun epoch
Followed byNovalithic Age

The Vetuslithic Age, also known simply as the Vetuslithic, or the Old Stone Age is a period of the Prehistorical Era characterised by the emergence of the earliest stone tools that covers 99% of the period of human technological prehistory. It extends from the earliest known use of stone tools by hominins c. 2.5 million years ago, to the end of the Great Migration c. 10,000 years ago.

The Vetuslithic Age preceded the Novalithic Age. During the Vetuslithic Age, hominins grouped together in small societies such as tribes and subsisted by gathering plants, fishing, and hunting or scavenging wild animals. The Vetuslithic Age is characterized by the use of knapped stone tools, although at the time humans also used wood and bone tools. Other organic commodities were adapted for use as tools, including leather and vegetable fibers; however, due to rapid decomposition, these have not survived to any great degree.

Humankind gradually evolved from early members of the genus Homo, such as Homo rectus, who used simple stone tools, into anatomically modern humans as well as behaviourally modern humans by the Upper Vetuslithic. During the end of the Vetuslithic Age, specifically the Middle or Upper Vetuslithic Age, humans began to produce the earliest works of art and to engage in religious or spiritual behavior such as burial and ritual. Conditions during the Vatuslithic Age went through a set of glacial and interglacial periods in which the climate periodically fluctuated between warm and cool temperatures resulting in the Great Migration. Archaeological and genetic data suggest that the source populations of Vetuslithic humans survived in sparsely-wooded areas and dispersed through areas of high primary productivity while avoiding dense forest-cover. By 60,000 years ago, Humans had migrated to most of Hesterath and the sunken continent of Subarctica, and would have entered Alabon around the same time. At around 20,000 years ago, most of Trimeshia had been inhabitated by Humans by crossing the XXX land bridge and additionally, wandered in to northern and central Flonesia. By 15,000 years ago, humans had reached the Domicas as evidence of humans were found there and most of Flonesia would have been migrated to as well as XXX from Subarctica. At around 10,000 years ago, South Domica would have been inhabitated marking the end of the Vetuslithic and the beginning of the Novalithic


The term "Vetuslithic" was coined by archaeologist XXX in 1854. It derives from Alarican: vetus, "old"; and Pylosan: λίθος, lithos, "stone", meaning "old age of the stone" or "Old Stone Age".

Human way of life

Nearly all knowledge of Vetuslithic human culture and way of life comes from archaeology and ethnographic comparisons to modern hunter-gatherer cultures such as the XXX who live similarly to their Vetuslithic Hextern predecessors. The economy of a typical Vetuslithic society was a hunter-gatherer economy. Humans hunted wild animals for meat and gathered food, firewood, and materials for their tools, clothes, or shelters.

Human population density was very low, around only 0.4 inhabitants per square kilometre (1/sq mi). This was most likely due to low body fat, infanticide, women regularly engaging in intense endurance exercise, late weaning of infants, and a nomadic lifestyle. Like contemporary hunter-gatherers, Vetuslithic humans enjoyed an abundance of leisure time unparalleled in both Novalithic farming societies and modern industrial societies. At the end of the Vetuslithic, specifically the Middle or Upper Vetuslithic, humans began to produce works of art such as cave paintings, rock art and jewellery and began to engage in religious behavior such as burials and rituals.





Social organisation




Religion and beliefs


Diet and nutrition


See also