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olavsu1 kirjutas: ↑13 Mär, 2023 9:13pole mõeldav, et põld rajataks ümber kivikülvi.

Põldur kirjutas: ↑13 Mär, 2023 9:32Kui te soovite, et kustutaksin selle postituse, kustutan.

Põldur kirjutas: ↑13 Mär, 2023 8:52Siin ütlevad, et need pole laibad seal. Et valeinformatsioon.
https://twitter.com/J_JHelin/status/163 ... GU27AtAAAA

Põldur kirjutas: ↑13 Mär, 2023 9:25 Ärge jääge kividesse kinni. Nad ju hiljem ütlevad, et need ei pruugi olla kivid.
Ma olen ka kursis, mis asi on mustmullavöönd. Aga nagu ütlesin, asukoht ja see, et need objektid olid seal juba 25 jaanuar ja , et ka kõrval põldudel on samu objekte, välistab, et need on laibad.

Luderi kirjutas: ↑13 Mär, 2023 9:52 Kas välistab sellega, et antud asukoht sellel ajal ei olnud lahingutegevuse tsoon või sellega et keegi ometigi ei jäta laipu mitmeks kuuks mädanema ja ei koristab enda järel ära?

speedsta kirjutas: ↑13 Mär, 2023 9:10 Kuidas mustmullavööndis üldse kividega lood? Pigem vist pole.

Kriku kirjutas: ↑13 Mär, 2023 9:22

olavsu1 kirjutas: ↑13 Mär, 2023 9:13pole mõeldav, et põld rajataks ümber kivikülvi.

Meil on selliseid põlde palju.

Aga ma kordan, vähemalt viimasest jääajast jäänud kivikülve ei saa Ukrainas olla. Mul pole praegu aega otsida, kas või millal Ukraina viimati jää all oli.

Last Glacial Maximum/Full Glacial (22,000 14C years ago) to 14,000 14C years ago. The last late Glacial from 22,000 up until just before 13,000 14C years ago was very cold and dry throughout Europe. Large ice sheets were present over much of northern Europe, and ice caps covered the Alps and the Pyrennes. Forest and woodland were almost non-existent, except for isolated pockets of woody vegetation in and close to the mountain ranges of southern Europe. Instead, a sparse grassland or semi-desert covered most of southern Europe, whilst a mixture of the dry, open 'steppe tundra' and polar desert covered the parts of northern Europe not occupied by ice sheets. Ice-wedge features suggest that permafrost extended across most of Europe, down to about the latitude of central France. Drifting sand and wind erosion were common in north and central Europe, and desert animals such as Saiga antelope were present as far west as France.

Various geomorphological, zoological, botanical and isotopic temperature indicators suggest that all parts of Europe were much colder than today, with the greatest cooling being in winter (Frenzel et al. 1992). At about the latitude of south-central Germany and north-western Ukraine, Frenzel (1992a) presents maps suggesting August mean temperatures of about 10-11 deg. Celsius, comparable with much of the northern coast of Siberia at present. Winter (February) mean temperatures were at least as low as -19 Celsius in central Germany and -27 Celsius across most of the Ukraine, the latter being similar to much of northern and central Siberia at present. In southern Europe, across most of the Mediterranean zone, temperatures were perhaps 8-10 degrees lower than at present in both summer and winter (Frenzel 1992 a,b).