Bøndene på Kvålehodlene : boplass-, jordbruks- og landskapsutvikling gjennom 6000 år på Jæren, SV Norge

In order to reconstruct the settlement-, agriculture- and land-use practises within the Kvåle-complex, Time municipality, in the Jæren region, an interdisciplinary project was organised in 2001-02. The approach involved archaeology, archaeobotany (macro- and microscopic plant remains) and soil studies (C/N-sampling). The archaeological and paleoecological results cover a long-term period, from the Late Mesolithic to Modern Times. Focus has been put on the neolithisation process and the shift in settlement pattern and agro-pastoral land-use until the Black Death (ca. 1350 AD). The settlement areas were uncovered by mechanical top-soil stripping. The ancient monuments linked to land-use, such as infields (clearance cairns, fields, lynchets, fences) and outfields (fences, ‘fairy-rings’, track-ways, offering stone) were documented on the basis of trenches and profiles. The Kvåle area is part of the hummocky moraine landscape in Jæren. In the Late Mesolithic this area was covered by broadleaved deciduous forest. Fragments of carbonised hazelnut shells demonstrate the stays of humans to be sporadic. Pollen analysis has documented forest clearance and animal husbandry ca. 3800 BC, and shows the increase of charcoal dust particles, non-arboreal pollen types and pollen from plants favoured by grazing. Throughout the 6000 years the landscape was transformed into a cultural environment of intensive cultivation. The next phase of human interference occur at the transition between the Late Neolithic and Early Bronze Age. At the eastern part of the main Kvåle hill bifacially retouched, triangular spearheads, flake-scrapers and cereals found against a large block split apart in two pieces, Lonaren, indicate ritual activities and offering. Postholes and hearths from at least three house foundations have been recovered on the westernmost ridge in the area. Two of the house structures, 14C dated to the Late Neolithic, ca. 1900-1700 BC, were two-aisled and measured 16.5 x 6 m to 23.0 x 7.2 m. In both the house structures were found large quantities of carbonised cereals, mainly emmer (Triticum dicoccum), naked barley (Hordeum vulgare var. nudum) and few seeds of weeds. Cereal cultivation in burnt and stony fields are documented in soil layers sealed by clearance cairns. The oldest clearance cairns are 14C dated to 1930-1780 BC. A third house structure, 14C dated to the Bronze Age period I, ca. 1700-1600 BC, was three-aisled and measured 16.8 x 5.7 m, and is among the oldest three-aisled house structures found in the Nordic area at present. In addition, the remains of two house structures of the two-aisled type, the youngest 14C dated to ca. 1600-1450 BC, underline the continuity of settlement. Together with traces of field clearance these are the earliest indications of a stable agropastoral society established locally in this period. Similar settlements are known in the Jæren region suggesting an overall agrarian expansion in the landscape. At the end of the Early Bronze Age clearance cairns were constructed on a large scale covering the main Kvåle hill. The agrarian landscape in the area developed into a mosaic of open birch forest, cleared-, grazed- and mown fields together with rotating small fields. A series of postholes and hearths from the Late Bronze Age and Early Pre-Roman Iron Age were found, but no distinct house foundations have been sorted out. In the Pre-Roman Iron Age the landscape covering the Kvåle complex was totally tree-less and heathland expanded. There were fields for cereal growing, grazing and mowing, but no distinction betweeninfield and outfield is apparent. A farm consisting of a 29 meters longhouse with outer stonewall, two burial mounds and fences are recorded from the Late Roman and Migration Ages. The habitation had been moved from the main Kvåle hill to the westernmost hill and lasted until 600 AD. Then the houses were abandoned, and the area was included in the outfields. In the Merovingian and Viking Ages small, rectangular lynchets were worked up and dispersed at the main Kvåle hill, due to an intense soil preparation followed by a secondary clearing of stones, sometimes recognised as stone strings in the lower part of the lynchets. At least two cultivation phases have been documented, the oldest 675-780 AD and the youngest 1015-1040 AD. Afterwards a new shift in the location of habitation appears, as postholes and hearts have been recorded, but the outline of houses could not be sorted out. The house structures date to the Viking Age and the Medieval Period. Hulled barley (Hordeum vulgare var. vulgare), oat (Avena) and a relatively high quantity of weed seeds dominate in the structures. In the beginning of the Medieval Period the dispersed pattern of several small, rectangular fields was contracted into one large lynchet, which was worked up by turf transported from the wetland. A thick soil layer developed and sealed older clearance cairns and field systems. Archaeobotanical material indicates that hulled barley (Hordeum vulgare var. vulgare), wheat (Triticum) and oat (Avena) were cultivated in this period. At the same time mowing has been documented at a southern hill by the construction of earthworks, such as haystacks (‘fairy-circles) in the outfields. After the Black Death the settlement was deserted and the fields were abandoned. The landscape remained open and was dominated by heathland up to the present

Sub-local differences in Late Holocene land use at Orstad, Jæren in SW-Norway, revealed by soil pollen stratigraphy

Made available with permission from Maney Publishing / Environmental Archaeology. www.maneypublishing.com/journals/env and www.ingentaconnect.com/content/maney/env.Four soil profiles along an 84 m transect through a clearance cairn field on podsol soils at Orstad, Jæren, SW Norway, were investigated. By relating pollen-analytical results to soil stratigraphical and morphological features, it was possible to reconstruct the landuse history of the site, and to reveal differences along the transect, although pollen preservation was poor. Human activity at Orstad began about 4500 uncalibrated 14C years BP. The reason for an intermediate abandonment of the site between about 4000 and 3600 uncalibrated 14C years BP was presumably a higher ground-water level, caused by local deforestation and/or by a climatic change. After that period, people seem to have grown cereals (Triticum and Hordeum) on at least two different field patches on the site. This land use was presumably occasional, and related to extraordinary needs. Fire-clearance seems to have been practised to prepare the fields for cultivation after long fallow periods. Between 2900 and 3200 uncalibrated 14C years BP, Orstad was possibly permanently inhabited. The agricultural fields were moved to higher levels, as the initial fields had become nutrient-depleted and too moist. Thin black layers in the profile may be remains of manure

Southwest Norway at the Pleistocene/ Holocene Transition: Landscape Development, Colonization, Site Types, Settlement Patterns

This is an electronic version of an article published in the Norwegian Archaeological Review© 2003 Copyright Taylor & Francis; Norwegian Archaeological Review is available online at http://www.tandfonline.com/doi/abs/10.1080/00293650307293.This article contributes a western Norwegian perspective to the ongoing debate on the timing and nature of the earliest colonization of northern Europe. Despite there being a theoretical possibility of Late Glacial settlement, currently available data indicate a populating of the area around the termination of the Pleistocene ca. 10,000 (uncalibrated) yr BP. The earliest radiocarbon date in southwest Norway so far, 9750 BP, is only a terminus ante quem. Environmental, economic, technological and social factors involved as a result of the colonization process are discussed briefly, and trends in the archaeological record are emphasized and commented on. The economy reflected by the first complete annual subsistence patterns is interpreted as having been logistically mobile, highly adaptive and generally of opportunistic character. Particular attention is paid to Early Preboreal coastal and inland settlement of the ‘Boknafjord’ and ‘Myrvatn/Fløyrlivatn’ groups, the latter characterized by well-preserved site structures such as tent rings and hearths providing high-resolution radiocarbon dates and palaeobotanical evidence