Sinu tööpäevad venivad sageli keskööni. Temperatuur ulatub 39,5-ni On läbinud kurgu ja nina testid. Murra tõiste muri.
Püssirohtu pudelisse, vett pääle ja pudelist loomale suhu kallata, nii et kõik rohu alla neelab. Kolm tikut haige looma nina juures korraga põlema tõmmata, seda arstimist korrata kolm kord järgemööda. Laaditi püss ainult rohuga, lasti kord vasemalt ja kord paremalt poolt kõhu alt läbi ning loom sai terveks.
Tulk, Mehis, Eelseisvate jäätmeveokonkursside tarvis on Saare maakonnas jäätmeloa hankinud lisaks OÜ-le Prügimees ka suured välismaised firmad Ragn-Sells ja Cleanaway. The stratigraphic sequence is divided by several unconformities reflecting tectonic movements which were connected with periods of extension of the depositional area. Two major phases and two minor events are recognized by the evaluation of the Pfalz SinoVaal poletiku uhise and the Lothringen unconformity, and the Leuter unconformity and the Saar unconformity, respectively.
The Lower Buntsandstein including Zechstein compries the first magnacycle and is built up of alluvial-fan deposits, fluvial braidplain sediments and marine to lagoonal deposits. Some aeolian sands as well as several palaeosols are also present.
The palaeolandscape consists of alluvial fans seaming Mida liigesed toodeldakse laanes margin of the basin and fluvial braidplains reaching from the toes of the fan belt to the centre of the depositional area which is occupied by a lagoonal sea that partially evolves into a playa-lake with progressive refreshment. The Middle Buntsandstein comprises the second magnacycle and is composed of an alternation of aeolian Dünnschichten and fluvial Felsbänke.
The third facies are alluvial-fan deposits of palaeogeographically restricted distribution along the margins of the basin. The aeolian Dünnschichten originate in the marginal parts of chott-type depressions in comparison with the recent Chott Djerid in Tunesia where rising ground water moistens the dry sediments that are laid down on the playa floor and thus allows their enhanced preservation.
In dry periods, wind-blown sand is spread out as plane sheets or as migrating wind ripple trains, or accumulates to barchanoid-type dunes that advance across the flat. Depending on supply of sand, all stages of transition between dune fields with only narrow interdune corridors between the ridges and interdune playas with isolated widely-spaced dunes are developed.