VSF 2010 Report - Nabo

More documents

Recommendations

Info

Taphonomy of the Faunal Assemblage Bone Fragmentation As is usually the case in Vatnsfjörður’s Viking age deposits, bones recovered from Area 14 are highly fragmented; complete bones are present in a very low percentage (± 1%). The degree of fragmentation of this collection resembles those recovered from the Viking Age area associated to structures and are consistent with assemblages produced by domestic activities (Dupont-Hébert <strong>2010</strong>). Figure 2. Distribution of faunal remains according to their fragmentation and level of completeness. 152
Combustion Traces Where previously excavated assemblages from soils in the vicinity of the Viking Age area had a high proportion of burnt bones related to propable field fertilisation, those associated with Structures 9 and 10 are less dominated by bones showing combustion traces (Figure 2). Figure 3. Relative frequency of combustion traces in the Viking age assemblages (U = unburnt bones; W = white bones, calcined through burning) Other Taphonomic Factors Other taphonomic traces, like gnawing and butchery marks, are mostly absent from this assemblage. Only one chop mark was identified on an ovi-caprine metapodial shaft. Bone cortex being affected by soil acidity might have played a role in the lack of those traces; bone surface modifications by chemical or mechanical weathering tend to cause the disappearance or misinterpretation of butchery marks. Trampling could also have occurred, resulting in bone fragmentation as shown in Figure 2. Some bone “powder” or “bone butter” was also noted in the assemblage and during the excavation. This almost total decompositin of the bone is probably related to the highly acidic (pH 4-5) and well-drained soils, which experience abundant rainfall and snowmelt, causing almost total leaching of calcium from the bone. Discussion The analysis of the whole Viking Age faunal assemblage should be done to optimize interpretation of the results. A better understanding of subsistence or economic strategies of 153
Page 1 and 2:
VATNSFJÖRÐUR 2010 FRAMVINDUSKÝRS
Page 3 and 4:
EFNI / CONTENTS Vatnsfjörður 2003
Page 5 and 6:
SAMANTEKT Garðar Guðmundsson Forn
Page 7 and 8:
Sem fyrr voru nemendur víða að,
Page 9 and 10:
tóbakspípum, ofnum og prjónuðum
Page 11 and 12:
q Borgarey Mjóifjörður Skálav
Page 13 and 14:
shown. Mynd/Figure 4. Stitched aeri
Page 15 and 16:
OVERVIEW Karen Milek University of
Page 17 and 18:
Summary of the Vatnsfjörður Resea
Page 19 and 20:
floor layer, and is likely to an ea
Page 21 and 22:
against the 3 m thick, external wes
Page 23 and 24:
• The digital terrain model of th
Page 25 and 26:
ÚTGEFNAR, SKÝRSLUR, RITGERÐIR OG
Page 27 and 28:
ERINDI UM VATNSFJÖRÐ PRESENTATION
Page 29 and 30:
ANNAÐ PUBLIC OUTREACH Opinn dagur
Page 31 and 32:
Excavation Methods The excavation o
Page 33 and 34:
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 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 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: Table 1. The 2010 Viking Age faunal
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
Page 183 and 184: Bibliography Bullock, P., Fedoroff,
Page 185 and 186: Figure 5.3 Description of Sample VS
Page 187 and 188: Figure 5.7 Description of Sample VS
Page 189 and 190: Figure 5.11 Description of Sample V
Page 191 and 192: Figure 5.16 Wood phytolith 50 µm F
Page 193 and 194: Figure 5.27 Iron Nodule (OIL) 100
Page 195 and 196: Betula pubescens (the native downy
Page 197 and 198: An opportunistic sampling strategy
Page 199 and 200: POLLEN ANALYSIS OF THE WET MEADOW A
Page 201 and 202: Figure 2. Site photograph detailing
Page 203 and 204:
to low percentages (
Page 205 and 206:
values were not a result of process
Page 207 and 208:
Figure 3. Pollen and spore percenta
Page 209 and 210:
CORRELATION OF TEPHRA LAYERS FROM V
Page 211 and 212:
and second, to ensure the most accu
Page 213 and 214:
Figure 2 . Geochemistry of Vatnsfj
Page 215 and 216:
Thorarinsson, S. (1955b). Nákuðun
Page 217 and 218:
10038 D 10010 Fill of post-hole [10
Page 219 and 220:
10569 C 10540 Post hole in hearth (
Page 221 and 222:
10632 D 8562 A midden deposit in ro
Page 223 and 224:
10054 D Lower horizon of land surfa
Page 225 and 226:
ÍS-204 Vatnsfjarðarsel/Seljaland/
Page 227 and 228:
ÍS-204:001C nokkurra metra kafla b
Page 229 and 230:
frá henni er Hólhúsótt [011] og
Page 231 and 232:
ÍS-204:032 Kálgarðsflöt gerði
Page 233 and 234:
sigið nokkuð inn í rústina fyri
Page 235 and 236:
... J vatzfirde fiorar merkur“ (D
Page 237 and 238:
ÍS-205:001 Vatnsfjörður bæjarh
Page 239 and 240:
grjótholti á breiðum hjalla. Var
Page 241 and 242:
norðnorðvestur-suðsuðaustur. Ha
Page 243 and 244:
ÍS-205:011 Nónvarða varða eykta
Page 245 and 246:
hólfum. Samtals er tóftin 8x7 m o
Page 247 and 248:
ÍS-205:021 hleðsla refagildra 655
Page 249 and 250:
ÍS-205:024 Mylluhóll heimild um m
Page 251 and 252:
verið rutt út. Talið er líklega
Page 253 and 254:
erfitt að greina lag hennar. Austa
Page 255 and 256:
ver um 11,5x5 m að innanmáli, þ
Page 257 and 258:
sóleyjum. Búið að slétta yfir
Page 259 and 260:
til vesturs. Op er á þeim hluta h
Page 261 and 262:
ÍS-205:047 varða óþekkt 6556.19
Page 263 and 264:
Vatnsfirði. Nokkrum metrum austan
Page 265 and 266:
ÍS-205:059 Að loknum uppgreftri v
Page 267 and 268:
gæti verið um holur til að elda
Page 269 and 270:
ÍS-205:068 varða óþekkt 6556.44
Page 271 and 272:
ÍS-205:076 Selsker varða óþekkt
Page 273 and 274:
ÍS-205:081 tóft útihús 6556.407
Page 275 and 276:
Norðaustan við íbúðarhúsið v
Page 277 and 278:
hún að hluta grafin niður. Garð
Page 279 and 280:
túnið til norðvesturs. Túngarð
Page 281 and 282:
Þústin samanstendur af grasþúst
Page 283 and 284:
ÍS206:032 heimild um kálgarð Um
Page 285 and 286:
hjallur norðvestan við fjós. Vi
Page 287 and 288:
Vatnið kemur úr litlu lækjarspr
Page 289 and 290:
ÍS-208:001 Hálshús bæjarhóll b
Page 291 and 292:
eru á þeim báðum í miðju, til
Page 293 and 294:
ÍS-208:012 gerði óþekkt 6554.97
show all

VSF 2010 Report - Nabo

Create successful ePaper yourself

Delete template?

Save as template?