2 years ago

As with the LCT collection retrieved from ES Lepolosi

In our model, we define Place B as a locale in which large implement configuration and use took place. Large flakes would arrive at these places in order to be transformed and used in specific tasks, although the production of usable medium-size f read more...

2 years ago

{Finally the sites of Wadi Surdud in Ca ndash nbsp cal nbsp BP

5.1.4. Ca 8600–8000 cal BP: maximum grassland expansion indicating wettest conditions of the sequence
Between ca 8500 and 8000 cal BP, Poaceae increase, to maximum frequencies of 34% (20–34%). In the younger, m read more...

2 years ago

Hitherto parking issues have received scant attention in the literature

This study was carried out among train users who parked a bicycle at Delft railway station in the Netherlands. Delft is a medium-sized university town in the Randstad, the economic core of the Netherlands (Maat & Louw, 2013). Its main railway read more...

2 years ago

Surface morphology and stratigraphy suggest that the fans have

Sediment for equivalent dose (De) estimate is most often collected by pounding a metal tube into a sand lens then removing it to retain an intact core of light-protected material. If the deposit is too compacted or cemented for a metal tube, it ma read more...

2 years ago

Table Field assay Exp pollen germination for two crop

Table 3.
Field assay (Exp. #2): pollen germination (%) for two crop Diphenyleneiodonium grown in field at increasing concent read more...

2 years ago

Soil temperature during disinfection treatmentsa in the Murcia greenhouse

Soil temperature during disinfection treatmentsa in the Murcia greenhouse experiments. Number of cumulative hours (h) in each temperature range. Data of all amendments are shown in year 2010 (treatment read more...

2 years ago

Fig nbsp xA The ratio of the chromatic aberration coefficient

Fig. 5. The ratio of the chromatic aberration coefficient to the spherical aberration coefficient Cc/CsCc/Cs of the quatric mirror for symmetric rays as a function of ν=(VA−VC)/(VA−VM)ν=(VA−VC)/(VA−VM). The soli read more...