• No results found

Landscape reconstruction

N/A
N/A
Protected

Academic year: 2022

Share "Landscape reconstruction "

Copied!
1
0
0

Bezig met laden.... (Bekijk nu de volledige tekst)

Hele tekst

(1)

System Begin End

A 100 BC 100 AD B 100 AD 750 AD

Database

Manual edited input Integrated time series

of landscape reconstruction

Script making time slices

Channels Tidal flats Tidal marshes

A

B B

A B

T = 50 AD

A

T = 500 AD

B

T = 1000 AD

B

A

Landscape reconstruction

Integration of data

Selection of settlements per time slice

ARCHIS

Additional regional overview studies

Source data

Archaeological settlements

EMA-D EMA-C EMA-B EMA-A

RP-L RP-M

RP-E

temporal resolution

EMA

1050 AD

450 AD

RP

12 BC

Integrated time slices of settlement data

T = 1000 AD

T = 500 AD

T = 50 AD

COASTAL REGION

GIS and database development (Pierik) Database development (Van Lanen)

+

+

1050 AD

450 AD

12 BC

> High ( ) Intermediate ( ) <

Sea ingression dynamics and occupation patterns in the Dutch coastal area during the first millennium AD

H.J. Pierik

1)

, R.J. van Lanen

1,2)

& E. Stouthamer

1)

1) Department of Physical Geography, Faculty of Geosciences, Utrecht University, Heidelberglaan 2, 3584 CS, Utrecht 2) Cultural Heritage Agency, Ministry of Education, Culture and Science, Smallepad 5, 3811 MG, Amersfoort

In many parts of the Netherlands the transition from the Roman period (RP) to the Early Middle Ages (EMA) coincided with declining population. This contribution explores landscape dynamics of the Dutch coastal area in the first millennium AD and its possible influences on occupation patterns.

To achieve this, we developed a GIS containing geological-geomorphological elements from tidal systems (channels, tidal flats and salt marshes). Knowledge on the geological development of the tidal systems is documented in the GIS allowing mapping of coastal evolution. By comparing these coastal- evolution maps with archaeological data, interaction between landscape changes and settlements

can be hypothesized. At the onset of the Early Middle Ages, first results suggest silting up of tidal inlets along the Dutch coast coinciding with an increased settlement density in the waning tidal areas.

Meanwhile, large-scale extension of tidal systems at the expense of habitable land occurred in the SW part of the Netherlands. Adversely, at the end of the Early Middle Ages the SW part of the Netherlands silted up and some large sea ingressions took place in the northern part of the Netherlands. In both of these regions the current archaeological data does not yet reveal a clear pattern.

Additional information:

Results

Methods

Cultural Heritage Agency of the Netherlands Ministry of Education, Culture and

Science

Other Beach barriers Active river channel belts (Rhine and Meuse) Brook valleys Settlements... Low chronological resolution (see map title) Higher chronological resolution (see map title)

Pa la eo ge og ra ph y: 8 0 B C Se ttl em en ts : R ed : 1 2 B C - 70 A D / B la ck : 1 2 B C - 45 0 A D Pa la eo ge og ra ph y: 1 10 A D Se ttl em en ts : R ed : 7 0 - 2 70 A D / B la ck : 1 2 B C - 45 0 A D Pa la eo ge og ra ph y: 2 85 A D Se ttl em en ts : R ed : 2 70 - 45 0 A D / B la ck : 1 2 B C - 45 0 A D Pa la eo ge og ra ph y: 5 50 A D Se ttl em en ts : R ed : 5 25 - 72 5 A D / B la ck : 4 50 - 10 50 A D Pa la eo ge og ra ph y: 8 85 A D Se ttl em en ts : R ed : 7 25 - 90 0 A D / B la ck : 4 50 - 10 50 A D Pa la eo ge og ra ph y: 1 05 0 A D Se ttl em en ts : R ed : 9 00 - 10 50 A D / B la ck : 4 50 - 10 50 A D

Outside the coastal area

Other Beach barriers Active river channel belts (Rhine and Meuse) Brook valleys Settlements... Low chronological resolution (see map title) Higher chronological resolution (see map title)

Pa la eo ge og ra ph y: 8 0 B C Se ttl em en ts : R ed : 1 2 B C - 70 A D / B la ck : 1 2 B C - 45 0 A D Pa la eo ge og ra ph y: 1 10 A D Se ttl em en ts : R ed : 7 0 - 2 70 A D / B la ck : 1 2 B C - 45 0 A D Pa la eo ge og ra ph y: 2 85 A D Se ttl em en ts : R ed : 2 70 - 45 0 A D / B la ck : 1 2 B C - 45 0 A D Pa la eo ge og ra ph y: 5 50 A D Se ttl em en ts : R ed : 5 25 - 72 5 A D / B la ck : 4 50 - 10 50 A D Pa la eo ge og ra ph y: 8 85 A D Se ttl em en ts : R ed : 7 25 - 90 0 A D / B la ck : 4 50 - 10 50 A D Pa la eo ge og ra ph y: 1 05 0 A D Se ttl em en ts : R ed : 9 00 - 10 50 A D / B la ck : 4 50 - 10 50 A D

Outside the coastal area Other Beach barriers Active river channel belts (Rhine and Meuse) Brook valleys Settlements... Low chronological resolution (see map title) Higher chronological resolution (see map title)

Pa la eo ge og ra ph y: 8 0 B C Se ttl em en ts : R ed : 1 2 B C - 70 A D / B la ck : 1 2 B C - 45 0 A D Pa la eo ge og ra ph y: 1 10 A D Se ttl em en ts : R ed : 7 0 - 2 70 A D / B la ck : 1 2 B C - 45 0 A D Pa la eo ge og ra ph y: 2 85 A D Se ttl em en ts : R ed : 2 70 - 45 0 A D / B la ck : 1 2 B C - 45 0 A D Pa la eo ge og ra ph y: 5 50 A D Se ttl em en ts : R ed : 5 25 - 72 5 A D / B la ck : 4 50 - 10 50 A D Pa la eo ge og ra ph y: 8 85 A D Se ttl em en ts : R ed : 7 25 - 90 0 A D / B la ck : 4 50 - 10 50 A D Pa la eo ge og ra ph y: 1 05 0 A D Se ttl em en ts : R ed : 9 00 - 10 50 A D / B la ck : 4 50 - 10 50 A D

Outside the coastal area

Conclusions

System Begin End

A 100 BC 100 AD B 100 AD 750 AD

Database

Manual edited input Integrated time series

of landscape reconstruction

Script making time slices

Channels Tidal flats Tidal marshes

A

B B

A B

T = 50 AD

A

T = 500 AD

B

T = 1000 AD

B

A

Landscape reconstruction

Integration of data

Selection of settlements per time slice

ARCHIS

Additional regional overview studies

Source data

Archaeological settlements

EMA-D EMA-C EMA-B EMA-A

RP-L RP-M

RP-E

temporal resolution

EMA

1050 AD

450 AD

RP

12 BC

Integrated time slices of settlement data

T = 1000 AD

T = 500 AD

T = 50 AD

COASTAL REGION

GIS and database development (Pierik) Database development (Van Lanen)

+

+

1050 AD

450 AD

12 BC

> High ( ) Intermediate ( ) <

Period Region Landscape Settlements

Roman Age North Small tidal systems silting up Severe settlement decline in LRP

West Tidal systems silting up Settlement concentration in silting up / silted up tidal areas South Large scale extension of the tidal area (S-Zeeland) Severe settlement decline in LRP

Early Middle Ages

North Small tidal systems silting up and

extension of 2 major tidal systems Sparse data

West Last tidal system (Rhine estuary) silting up Settlement concentration in silting up / silted up tidal areas South Large scale extension tidal area (N-Zeeland) /

tidal flats silt up to become marshes (S-Zeeland) Minor settlement increase

T = 1000 AD

T = 500 AD

T = 50 AD

Project website Poster pdf References

Other

Beach barriers

Active river channel belts (Rhine and Meuse) Brook valleys

Settlements...

Low chronological resolution (see map title) Higher chronological resolution (see map title)

Palaeogeography: 80 BC

Settlements: Red: 12 BC - 70 AD / Black: 12 BC - 450 AD Palaeogeography: 110 AD

Settlements: Red: 70 - 270 AD / Black: 12 BC - 450 AD Palaeogeography: 285 AD

Settlements: Red: 270 - 450 AD / Black: 12 BC - 450 AD

Palaeogeography: 550 AD

Settlements: Red: 525 - 725 AD / Black: 450 - 1050 AD Palaeogeography: 885 AD

Settlements: Red: 725 - 900 AD / Black: 450 - 1050 AD Palaeogeography: 1050 AD

Settlements: Red: 900 - 1050 AD / Black: 450 - 1050 AD

Outside the coastal area

Schelde

Meuse

Rhine

Oer-IJ

Vlie Boorne

Middelzee

Paesens Hunze

Schelde

Meuse

Rhine

Vlie

Middelzee

Lauwers

Eems

Honte

Grevelingen Fivel

Eems

Schelde

Meuse

Rhine

Vlie Boorne

Middelzee

Hunze Fivel

Eems

Meuse

Rhine

Vlie Boorne

Middelzee

Hunze Fivel

Eems

Meuse

Rhine

Schelde

Honte

Vlie Boorne

Middelzee

Hunze Fivel

Eems

Schelde

Honte

Schelde

Meuse

Rhine

Vlie

Middelzee

Lauwers

Eems

Honte

Grevelingen

inherited from Early Holocene/Late Pleistocene estuary

newly formed (sea ingression) Tidal inlet systems

Referenties

GERELATEERDE DOCUMENTEN

The main goal of this research will thereby be to examine the financial feasibility of implementing the discussed solution in the area of the Grevelingen &amp; Krammer-Volkerak

The petrographic study of 56 sherds, the chemical analysis of 40 samples, and XRD study of 12 of them coming from 4 sites reach the changes of the process between the two time

214 Altogether, as Anne Duggan formulated it, 'Becket's began as a spontaneous cult which grew rapidly, inspired by belief that his death had been a martyrdom, and

The guest book notes of the five churches analyzed in this study are personal messages written by visitors about their experiences with a specific church monument.. These notes

After relating individual degrees of attrition to the degree of fusion of epiphyses and sutures we established a sequence of estimated ages at death (see tab. All the adults had

Unexplored until the recent excavation campaign, except for a small sounding excavated during the 1990s by the Joint Hadd Project (JHP), the Um An Nar site of RJ-3 most

The pres- ence of these sites, combined with mounting evidence from geoarchives of human impact on the landscape since the neolithic, has led us to investigate the settlement

The first crops produced in the Aisne valley comprise naked barley (Hordeum vulgate var. nudum), emmer wheat (Triticum dicoccum), einkorn wheat (Trilicum