Troszke zdjec z dzisiejszej wyprawy (Li and Ra) na znajdujace sie w poblizu nas Celtic Fields.. To moja pierwsza wizyta w tym miejscu.. w odroznieniu do Celtic Sands, znajdujacych sie blizej parku, ktore odwiedzalam juz niejeden raz i o ktorych wspominalam chocby w notce

Celtic Fields, choc jakos i do nich bardziej pasuje mi nazwa – Celtic Sands.. to doslownie prawdziwe pola piasku.. i pejzaz wprost niesamowity… aah.. mozna wpasc w piaszczysty trance.. przywodzacy mi troszke na mysl krajobraz polskiej Leby, a troszke Hel.. podobny typ roslinnosci, etc… takie moje pierwsze skojarzenia… a ponadto Diune.. tyle, ze tutaj do morza dosc daleko… w koncu to centralna Holandia..

my HollyLand..

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ponizej cos w j. ang na temat tego miejsca

Drivers of drift sand dynamics; a reconstruction for the Wekeromse Zand, the Netherlands

Sonneveld, M.P.W.; Hendriks, C.J.M.; Wallinga, J.

Summary

Inland active drift sand landscapes are regarded as unique ecosystems of great historical and geomorphological value. Recent studies have highlighted the role of multiple factors in the initiation and stabilization of drift sand landscapes. To unravel the importance of different forcings (e.g. agricultural practices, climate) and their interplay, insight in the chronology of drift sand dynamics is essential.In this study, we aimed to reconstruct the dynamics of the drift sand landscape of the Wekeromse Zand (central Netherlands) and to develop a conceptual model to understand the processes involved. The Wekeromse Zand study area is located on the border of a central push moraine and is characterised by open active drift sands and vegetated hills and valleys. The surroundings are dominated by modern agricultural practices, and remnants from ancient iron age Celtic Field systems. For the study area we: i) analysed historical maps going back to the early 19th century, ii) performed a field survey to map the palaeolandscape (before drift sand activation) and iii) employed optically stimulated luminescence (OSL) dating of drift sand deposits on 11 samples from two locations to determine the timing of drift sand deposition. Analysis of the available topographic maps showed no substantial aeolean activity of the area outside its morphological boundaries. OSL dating revealed that two drift sand layers were deposited between 1373 and 1462 AD and between 1680 and 1780 AD. The Wekeromse Zand has known three relatively stable periods: i) a period between the start of the Holocene to the Late Medieval Period, ii) in between the Medieval climatic optimum and the climatic Maunder minimum, and iii) current situation. The two active phases appear to correspond with active phases in the coastal dune systems and are probably the combined result of anthropogenic land use and climatic changes.

https://www.wageningenur.nl/en/Publication-details.htm?publicationId=publication-way-343433393732

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to jedna z bardziej zielonych wysepek posrod morza piasku

i moja spowiedz.. do drzewa

w pelni sekretna..

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a nurkujac ponownie w sand sea..

poczulam aby na jego ”dnie”narysowac ot po prostu – serce…. z rozchodzaca sie falowo energia.. tak naprawde symbolizujace aqa*** sun…

i wtedy – poprzez ten piaskowy ryt – poczulam bardzo glebokie polaczenie z north sea…

jakby poplynal strumien ozywiajacej energii…

from heart to heart

❤

a tu piasek naturalnie uformowany wmorskie fale

co jeszcze lepiej widacpo zmianie koloru z sand na blue

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ponizej celtic sands z duzego przyblizenia

niby ”zwykły piasek kwarcowy” a ile w nim piekna.. po prostu krysztalowe cudenka..

i love sand

❤

a to Ra kreujacy swoj sand draw

a juz w drodze powrotne zatrzymalo mnie przy sobie na nieco dluzej inne miejsce.. nieco wyzszy piaszczysty wzgorek.. bedacy troszke jak kurhan.. bardzo energetyczny punkt, w ktorym narysowalam inne serduszko i juz na sam koniec dodalam magiczne