VSF 2010 Report - Nabo

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Problems and Potential The practice of coring can help identify the extent of archaeological features or locate them, although some difficulties can emerge. First, the stratigraphy released by this exercise represent only a small sample of the whole feature and could eventually represent a single event (like postholes or small hearth feature). Second, in the case of middens, only bone fragments are seen in cores due to its width and therefore it is difficult to estimate with certainty bone preservation and real archaeological potential of the feature. Third, in the case of Vatnsjarðasel and Hálshús, the peat ash and charcoal deposits, having almost no inclusion, can illustrate the burning of peat used as fuel. Also, because peat ash is a threat to bone preservation, faunal remains could have been destroyed by chemical action (acidity). Finally, the depth that can be reached by the tool is limited and therefore full extent of feature can be missed. Nonetheless, coring is a usefull way to discern differences between natural and anthropogenic depositions, and to characterize stratigraphy on a large scale basis with little site impacts, minimum effort and labour. Bibliography Aldred, Oscar (2007) Landscape Reseach in the Vatnsfjörður Environs, in Milek K. (ed.) Vatnsfjöður 2007 Framvinduskýrslur/Interim <strong>Report</strong>, FS383-03097. Fornleifastofnun Íslands, Reykjavík, pp. 21-42. JÁM VII (1984) Jarðabók Árna Magnússonar og Páls Vídalíns VII. Ísafjarðar-og Strandasýsla,Hið Íslenska Fræðafjélag, Kaupmannahöfn. 86
silo Main turf building #1 Test #3 #2 #4 Top soil and sub soil Silt Charcoal lenses Turf LEGEND Core location Structures Sketched topographic curves Peat ash Possible midden location N C. Dupont-Hébert, 2011 Figure 4. Sketch of Vatnsjarðasel farm with coring locations and results 87
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VATNSFJÖRÐUR 2010 FRAMVINDUSKÝRS
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EFNI / CONTENTS Vatnsfjörður 2003
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SAMANTEKT Garðar Guðmundsson Forn
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Sem fyrr voru nemendur víða að,
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tóbakspípum, ofnum og prjónuðum
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q Borgarey Mjóifjörður Skálav
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shown. Mynd/Figure 4. Stitched aeri
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OVERVIEW Karen Milek University of
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Summary of the Vatnsfjörður Resea
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floor layer, and is likely to an ea
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against the 3 m thick, external wes
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• The digital terrain model of th
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ÚTGEFNAR, SKÝRSLUR, RITGERÐIR OG
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ERINDI UM VATNSFJÖRÐ PRESENTATION
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ANNAÐ PUBLIC OUTREACH Opinn dagur
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Excavation Methods The excavation o
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Occupation Phases of Structure 10 S
Page 35 and 36: Upon the removal of the gravel plat
Page 37 and 38: EXCAVATIONS IN THE FARM MOUND AREA
Page 39 and 40: The Excavations Group 10662 Group (
Page 41 and 42: Associated with turf blocking [1050
Page 43 and 44: contained similar finds as were fou
Page 45 and 46: The removal of the deposits excavat
Page 47 and 48: sherds, a possible indication of th
Page 49 and 50: Figure 11. An overview of extension
Page 51 and 52: Group 9502 Group (9502) contains de
Page 53 and 54: In 2010 the area was extended to th
Page 55 and 56: Figure 16. An overview of room (106
Page 57 and 58: Group 10590 Group (10590) is a 7m l
Page 59 and 60: At the end of the 2010 season it ha
Page 61 and 62: Figure 21. Wall [10644]. Facing eas
Page 63 and 64: 17th - 18th century 1906 disturbanc
Page 65 and 66: Descriptions of Sections Trench 42
Page 67 and 68: a b Figure 3. South-facting section
Page 69 and 70: EVALUATION TRENCHES EXCAVATED AT VA
Page 71 and 72: Trench 37 Around 20 m south-west of
Page 73 and 74: glazed ceramics, burnt stone, windo
Page 75 and 76: luish-grey layer of coarse sand [10
Page 77 and 78: This was thought to be an indicatio
Page 79 and 80: Table 1. Register of units recorded
Page 81 and 82: CORING AT HÁLSHÚS AND VATNSFJARÐ
Page 83 and 84: Visible structure #5 #4 #2 #3 #1 Po
Page 85: Vatnsfjarðasel Vatnsfarðasel is l
Page 89 and 90: 29-38 cm same as above 38-39 cm cha
Page 91 and 92: 63-74 cm same as above 74-76 cm lam
Page 93 and 94: 53-57 cm laminated reddish brown, l
Page 95 and 96: Organic preservation was generally
Page 97 and 98: ASSESSMENT AND EVALUATION OF THE AR
Page 99 and 100: depth has been written about the di
Page 101 and 102: using an ISIS ABT-55 scanning elect
Page 103 and 104: Smithing Hearth Bottom During the p
Page 105 and 106: Fingers, or ‘tendrils’ of flowe
Page 107 and 108: Classification Counts Weight (kg) u
Page 109 and 110: Conversely, the small size of undia
Page 111 and 112: Microscopy The results from the opt
Page 113 and 114: that iron production and smithing w
Page 115 and 116: would be a worthy pursuit. The lack
Page 117 and 118: Milek, K. (2009). Excavations in th
Page 119 and 120: Archaeometallurgy, eds. S. L. Niece
Page 121 and 122: Table 2. Showing the size, weight a
Page 123 and 124: Table 4. Showing the dimensions and
Page 125 and 126: Figure 3. A 3-Dimensional bar chart
Page 127 and 128: Figure 5. Photographs of two ‘fun
Page 129 and 130: Figure 9. Examples of technical vit
Page 131 and 132: Figure 12. BSE image of smelting sl
Page 133 and 134: Figure 16. Optical micrograph of un
Page 135 and 136: Figure 20. Photographs of the ten p
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Appendix 1: Abbreviations Undiagnos
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Hammerscale Ferruginous concretions
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pebbles of dense vesicular basalt,
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ID. [324] Mag. Max. Dimensions (cm)
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mixed with the small undiagnostic s
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ID. [6103] Mag. Max. Dimensions (cm
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ID. [...] Finds No. Class. Count We
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Table 1. The 2010 Viking Age faunal
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Combustion Traces Where previously
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BOTANICAL REMAINS FROM A SAMPLE COL
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Figure 1. West-facing section of sa
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Some bioturbation by roots and worm
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300 Charcoal Volume (ml)/Number Sea
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Discussion Origin of Charcoal As me
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driftwood. All of the driftwood col
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Changes in Charcoal and Seaweed Con
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above the farm, and the two specime
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FRIÐRIKSSON, A. & TULINIUS, T.H. (
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SOIL MICROMORPHOLOGY ASSESSMENT OF
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suggesting that this side of the bu
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Figure 2b. Structure 3 in 2006 faci
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occupation deposit. The floor layer
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the structure dry by digging down t
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Bibliography Bullock, P., Fedoroff,
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Figure 5.3 Description of Sample VS
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Figure 5.7 Description of Sample VS
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Figure 5.11 Description of Sample V
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Figure 5.16 Wood phytolith 50 µm F
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Figure 5.27 Iron Nodule (OIL) 100
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Betula pubescens (the native downy
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An opportunistic sampling strategy
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POLLEN ANALYSIS OF THE WET MEADOW A
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Figure 2. Site photograph detailing
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to low percentages (
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values were not a result of process
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Figure 3. Pollen and spore percenta
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CORRELATION OF TEPHRA LAYERS FROM V
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and second, to ensure the most accu
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Figure 2 . Geochemistry of Vatnsfj
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Thorarinsson, S. (1955b). Nákuðun
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10038 D 10010 Fill of post-hole [10
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10569 C 10540 Post hole in hearth (
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10632 D 8562 A midden deposit in ro
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10054 D Lower horizon of land surfa
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ÍS-204 Vatnsfjarðarsel/Seljaland/
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ÍS-204:001C nokkurra metra kafla b
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frá henni er Hólhúsótt [011] og
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ÍS-204:032 Kálgarðsflöt gerði
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sigið nokkuð inn í rústina fyri
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... J vatzfirde fiorar merkur“ (D
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ÍS-205:001 Vatnsfjörður bæjarh
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grjótholti á breiðum hjalla. Var
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norðnorðvestur-suðsuðaustur. Ha
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ÍS-205:011 Nónvarða varða eykta
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hólfum. Samtals er tóftin 8x7 m o
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ÍS-205:021 hleðsla refagildra 655
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ÍS-205:024 Mylluhóll heimild um m
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verið rutt út. Talið er líklega
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erfitt að greina lag hennar. Austa
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ver um 11,5x5 m að innanmáli, þ
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sóleyjum. Búið að slétta yfir
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til vesturs. Op er á þeim hluta h
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ÍS-205:047 varða óþekkt 6556.19
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Vatnsfirði. Nokkrum metrum austan
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ÍS-205:059 Að loknum uppgreftri v
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gæti verið um holur til að elda
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ÍS-205:068 varða óþekkt 6556.44
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ÍS-205:076 Selsker varða óþekkt
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ÍS-205:081 tóft útihús 6556.407
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Norðaustan við íbúðarhúsið v
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hún að hluta grafin niður. Garð
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túnið til norðvesturs. Túngarð
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Þústin samanstendur af grasþúst
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ÍS206:032 heimild um kálgarð Um
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hjallur norðvestan við fjós. Vi
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Vatnið kemur úr litlu lækjarspr
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ÍS-208:001 Hálshús bæjarhóll b
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eru á þeim báðum í miðju, til
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ÍS-208:012 gerði óþekkt 6554.97
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VSF 2010 Report - Nabo

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