VSF 2010 Report - Nabo

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Figure 14. BSE image of smelting slag showing a distinct transgranular crack dividing two distinct zones. Above the fracture is characterized by fine dendritic wūstite, whereas the area below is densely populated with larger rounded and knobbly grains of globular wūstite x40. Figure 15. Optical micrograph of undiagnostic slag showing globular wūstite (some dendritic structures) embdeed in a matrix of polycrystalline fayalite (mid-grey) and glass (dark grey). Unetched, PPL, x100. 132
Figure 16. Optical micrograph of undiagnostic slag showing fused material with obvious mineralic inclusions. PPL, x100. Figure 17. BSE image of undiagnostic slag fragment showing the semi-fused structure containing mineralic inclusions. The structure has also taken on the cellular structure of some vegetatious elements, which have preliminarily been identified as conifer. x100. 133
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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
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luish-grey layer of coarse sand [10
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This was thought to be an indicatio
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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 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: Figure 12. BSE image of smelting sl
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
Page 177 and 178: Figure 2b. Structure 3 in 2006 faci
Page 179 and 180: occupation deposit. The floor layer
Page 181 and 182: 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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