VSF 2010 Report - Nabo

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Figure 4. Photographs of a selection of tap slag fragments and accumulations. 126
Figure 5. Photographs of two ‘funnel-shaped’ slag accumulations, illustrating the assumed flow direction from the ‘spout’ feature, tapering outwards. Figure 6. Photographs of a ‘funnel-shaped’ slag accumulation with the ‘spout’ feature, tapering outwards. 127
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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
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Upon the removal of the gravel plat
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EXCAVATIONS IN THE FARM MOUND AREA
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The Excavations Group 10662 Group (
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Associated with turf blocking [1050
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contained similar finds as were fou
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The removal of the deposits excavat
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sherds, a possible indication of th
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Figure 11. An overview of extension
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Group 9502 Group (9502) contains de
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In 2010 the area was extended to th
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Figure 16. An overview of room (106
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Group 10590 Group (10590) is a 7m l
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At the end of the 2010 season it ha
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Figure 21. Wall [10644]. Facing eas
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17th - 18th century 1906 disturbanc
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Descriptions of Sections Trench 42
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a b Figure 3. South-facting section
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EVALUATION TRENCHES EXCAVATED AT VA
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Trench 37 Around 20 m south-west of
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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 and 86: Vatnsfjarðasel Vatnsfarðasel is l
Page 87 and 88: silo Main turf building #1 Test #3
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: Figure 3. A 3-Dimensional bar chart
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
Page 137 and 138: Appendix 1: Abbreviations Undiagnos
Page 139 and 140: Hammerscale Ferruginous concretions
Page 141 and 142: pebbles of dense vesicular basalt,
Page 143 and 144: ID. [324] Mag. Max. Dimensions (cm)
Page 145 and 146: mixed with the small undiagnostic s
Page 147 and 148: ID. [6103] Mag. Max. Dimensions (cm
Page 149 and 150: ID. [...] Finds No. Class. Count We
Page 151 and 152: Table 1. The 2010 Viking Age faunal
Page 153 and 154: Combustion Traces Where previously
Page 155 and 156: BOTANICAL REMAINS FROM A SAMPLE COL
Page 157 and 158: Figure 1. West-facing section of sa
Page 159 and 160: Some bioturbation by roots and worm
Page 161 and 162: 300 Charcoal Volume (ml)/Number Sea
Page 163 and 164: Discussion Origin of Charcoal As me
Page 165 and 166: driftwood. All of the driftwood col
Page 167 and 168: Changes in Charcoal and Seaweed Con
Page 169 and 170: above the farm, and the two specime
Page 171 and 172: FRIÐRIKSSON, A. & TULINIUS, T.H. (
Page 173 and 174: SOIL MICROMORPHOLOGY ASSESSMENT OF
Page 175 and 176: 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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