VSF 2010 Report - Nabo

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Figure 3. Structure (10662) at the end of the 2009 field season. Facing north-east. The 2010 excavations revealed three more phases of the structure (subgroups 9650, 10663, 10664), defined by minor changes such as additions to walls and blockings, the latest being group (9650) and the earliest group (10664). The 2010 excavations also established that the structure could in all likelihood be dated to late 17 th -or early 18 th century. The south-east corner if this structure had been truncated by an early 20 th century vegetable garden, group 8590, referred to in the 2009 report as the “middle area” (Gísladóttir in Milek 2010,72-73. See also discussion on group 8590, below). Group (9650) Group (9650) contains deposits belonging to the second-latest phase of structure (10662) and is defined by a turf blocking, unit [10509], which partially sealed its north entrance. 40
Associated with turf blocking [10509] was one dark floor deposit, up to 25 cm thick, (unit [9633]), excavated in 2009. This covered most of the interior of the structure. This floor deposit was heavily organic and seemed to be composed of animal waste and remains of hay and contained pieces of bones, wood and textiles. The organic nature of the floor was the main reason for the 2009 assumption that the structure was the remains of sort of dwelling for animals. Immediately under floor [9633], concentrated in the northwest and north-east corner of the structure, were two levelling deposits, [10505] and [10507], both composed of turf and stone. It is possible that these deposits were the foundations for wooden structures, possibly mangers. 0m N [10509] [10505] [10507] (Gr.9650) (Gr.10515) (Gr.8590) (Gr.10590) 10m (Gr. 9502) Stones Turf (Gr.8562) Figure 4. A simplified drawing of phase (9650) of structure (10662). The half blocked north entrance of the structure led to a front room covered with three firm levelling or floor deposits that were clearly associated with blocking [10509] (in chronological order youngest - oldest: [10504], [10506], [10512]). All of these deposits were composed of large stones and turf, but were heavily mixed with charcoal which might indicate the proximity to a hearth. In the earliest of these, deposit [10506], a sherd of 17 th century pottery was recovered, and furthermore when turf blocking [10509] was removed, the bowl of a 17 th century clay pipe was found at its base, an indication that the structure could be dated to that period. Excavations in the north-west corner of the research area confirmed this, when it became clear that the western wall of structure [10662] was sealed by the in situ tephra from the 1693 eruption in Mount Hekla in southern Iceland (see group 41
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: The Excavations Group 10662 Group (
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
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63-74 cm same as above 74-76 cm lam
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53-57 cm laminated reddish brown, l
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Organic preservation was generally
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ASSESSMENT AND EVALUATION OF THE AR
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depth has been written about the di
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using an ISIS ABT-55 scanning elect
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Smithing Hearth Bottom During the p
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Fingers, or ‘tendrils’ of flowe
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Classification Counts Weight (kg) u
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Conversely, the small size of undia
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Microscopy The results from the opt
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that iron production and smithing w
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would be a worthy pursuit. The lack
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Milek, K. (2009). Excavations in th
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Archaeometallurgy, eds. S. L. Niece
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Table 2. Showing the size, weight a
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Table 4. Showing the dimensions and
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Figure 3. A 3-Dimensional bar chart
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Figure 5. Photographs of two ‘fun
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Figure 9. Examples of technical vit
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Figure 12. BSE image of smelting sl
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Figure 16. Optical micrograph of un
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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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