Gampelen/Rundi, Mesolithic sites on a sand dune in the Swiss `Seeland´.

View over the Rundi dune, Gampelen during the test-trenching campaign for the AD Bern. September 2015.

Sand. Like the sand in a sand box. No stones, no clay nor silt, just beautiful yellow sand. My very first dig was in the southern Netherlands and the soil consisted solely of sand. And it was great! I then spend a number of years digging in sand and I guess, it became my first archaeological “home-soil”. I have since dug in many countries and even more soil types and let me tell you, digging is never faster as in sand. I am not saying there are no challenges in understanding the stratigraphy and archaeology, but it truly is very handy. So when I got a phone call if I wanted to do some test-trenching in a sandy area in Switzerland I was quite keen. When I heard it was in Gampelen, where a number of Mesolithic surface concentrations have been long known and one – Jänet 3 – has been excavated, I was sold!

Two chipped stone tools from Gampelen, Jänet 3 (surface finds), found by H. Stucki. From Cornelissen, in Archäologie Bern, 2015. Drawings: Chr. Rungger (AD Bern).

I took a few months off from the big PhD and although we did not find much archaeology in the way of finds and structures, we did find some and we were also able to firmly establish the edge of the Lac de Neuchâtel here during the Mesolithic. Besides, it was very good to be able to take some distance from the PhD-work for a short while. The surface scatters in the vicinity of our test trenches we now know were, like Jänet 3, situated near small depressions on top of Aeolian sand dunes. In these depressions might have either stood open water or moors. From the stratigraphy it is now also clear that not all finds have been ploughed up yet and some of the archaeology might still be preserved in-situ. So, in a way it turned out to be more of a landscape archaeological project than your average Meso-dig. Since then dendro-archaeologist Matthias Bollinger and the WSL have also established that much of the sand of the Rundi dune must have been deposited in the 10th Millennium BC. Moreover, the wood samples we took during the test-trenching will help to extend the dendrochronological curve of the area a bit further towards the Late Glacial period. And all of that from that lovely sand in the Seeland!

We even made it on the cover of “Archäologie Bern 2015”!

It was photographer Heini Stucki who originally discovered these sites and he has been field walking here the past 30 odd years. The full test-trenching report has now been published and also includes the surface finds from the past decade. A short summery of the results was also published as a “Fundbericht” in the Annuaire d’Archaéologie Suisse 98, 2015.

And when you’re finished looking up the Gampelen report, do have a look at Heini Stucki’s website and his beautiful photos as well!

(With many thanks to the mighty Rolf W.!)

References:

Cornelissen, M., 2015, Gampelen, Rundi und Jänet. Eine mesolithische Dünenlandschaft am Neuenburgersee. In Archäologie Bern / Archéologie bernoise. Jahrbuch des Archäologischen Dienstes des Kantons Bern 2015 / Annuaire du Service archéologique du canton de Berne 2015. Bern, Arch. Dienst Kanton Bern. Pp. 64-67. ISBN 978-3-907663-48-6.    (Zu beziehen in Buchhandlungen oder bei Verlag RubMedia, Tel. 031 380 14 80.)

Cornelissen, M., 2015, Gampelen BE, Rundi. Annuaire d’Archéologie Suisse 98.  Pp. 176-7.

Nielsen, E., 1991, Gampelen – Jänet 3. Eine mesolithische siedlungsstelle im westlichen Seeland. Bern, Staatlicher Lehrmittelverlag.

Pinus cembra, Tamangur, Las Gondas and the Mesolithic

“The Stone pine, each its own, unmistakable: born and growing on this very spot, while birds came and moved along and other birds came and left again. And she has turned old, ancient, she became ever more beautiful, more free, whether you look at her or not, one day she will die up here, torn by fire, thrown down by the dry hot föhn-wind, with her trunk hollow of age which will lie pale as bone, with its blunt branches, bumbs and horns on her almost indistructable patriarchical body.”

Andri Peer. «Daman da chatscha» / «Jagdmorgen» (1959/1961); my translation.

In German:

«Die Arve, jede sich selbst, unverwechselbar: geboren und gewachsen auf diesem Platz, während die Vögel gekommen und fortgezogen sind und andere Vögel gekommen und wieder gegangen. Und sie ist alt geworden, uralt, immer schöner, immer freier, ob du sie anschaust oder nicht, eines Tages stirbt sie hier oben, zerrissen von einer Feuerpranke, zu Boden geworfen vom Föhn, mit dem vor Alter schon hohlen Stamm, der noch Jahre und Jahre rein erbleicht mit seiner Knochenweisse, mit seinen stumpfen Ästen, Buckeln und Hörnern auf dem fast unverweslichen Patriarchenleib.»

Andri Peer. «Daman da chatscha» / «Jagdmorgen» (1959/1961)

In Peer’s text this magnificent stone pine, Pinus cembra (also known as the Arolla or Swiss stone pine) might stand as a symbol for the Romansh languange and culture and its perserverence (ca. 60.000 people speak one of its dialects). It reminds me of the piece of wood that was cut from a trunk in an alpine moor at 2363 masl in Las Gondas. The Las Gondas moor lies just below the Fuorcla da Tasna, above the Lower Engadin valley. Because a sample taken from the tree trunk could be dendrochronologically dated, we know it grew and grew old here over eight and a half thousand years ago. But already almost 2000 years before that Arolla pine grew here, as needles from that time have been found in the Las Gondas moor.

If you have never been there, you should visit the Tamangur forest on the southern side of the Lower Engadin valley. It is fantastic to walk through this open forest high in the Alps, a forest made up almost exclusively of Stone pines. Alive there is a softness about them, with their many small bundles of each five needles. But they can also appear almost archaic, their bare roots arching into the soil below. There is not much undergrowth, low bilberry bushes and alpenroses, the ground soft with needles, moss and grass.

Die knochenweissen Arven von Sursass, im Hintergrund der Piz Lindard bei Lavin. (Foto: Rudolf Grass, Zernez) Bild: Simon Schmid Aus Ganzoni in Der Bund 02.01.2015

Tamangur forest is one of the last of its kind. I am at the moment trying to write an article about the Mesolithic of the Alps of southeastern Switzerland. We know that 10’000 years ago, with the glaciers still retreating, people were already at similar altitudes not far from Las Gondas and they might well have walked in the cool shade of the very Stone pines that shed their needles and left their trunks in Las Gondas. They might have sheltered under the enormous rocks in the Plan da Mattun and have rested on the bare, bleached bone roots and trunks of these ancient trees.

Literature:

Dietre, B., Walser, C., Lambers, K., Reitmaier, T., Hajdas, I., Haas, J.-N., 2014. Palaeological evidence for Mesolithic to Medieval climatic change and anthropogenic impact on the Alpine flora and vegetation of the Silvretta Massiv (Switzerland/Austria). Quarternary International 353, 3-16.

Ganzoni., A., 2015, Aufgetaucht: «Das verborgenere Engadin». Fundstücke aus dem Schweizerischen Literaturarchiv: Eine Fotokarte des Engadiner Schrifstellers Andri Peer, in: Der Bund 02.01.2015  (last visited 16.01.2015)

Nicolussi, K., 2012. Jahrringdaten zur Früh- und mittelholozänen Baumgrenze in der Silvretta, in: Reitmaier, T. (Ed.), Letzte Jäger, Erste Hirten. Hochalpine Archäologie in der Silvretta. Amt für Kultur, Archäologischer Dienst Graubünden, Chur, pp. 87-100. (PDF of an older version).

Reitmaier, T., 2012. Letzte Jäger, erste Hirten. Alpine Archäologie in der Silvretta 2007-2012, in: Reitmaier, T. (Ed.), Letzte Jäger, erste Hirten. Hochalpine Archäologie in der Silvretta. Amt für Kultur, Archäologische Dienst Graubünden (ADG), Chur, pp. 9-65.