Sie suchten nach: appalachian (Tschechisch - Englisch)

"the appalachian photographs."
"the appalachian photographs."

"the appalachian photographs of doris ulmann".
"the appalachian photographs of doris ulmann".

"photographs of appalachian craftsmen: a retrospective exhibition, april 6-may 1, 1976".
"photographs of appalachian craftsmen: a retrospective exhibition, april 6-may 1, 1976".

přezkum epa arch coal navrhovaného smrk 1 projekt v západní virginii uvedl, že projekt nemohl být převedeny bez nepříznivých dopadů na okolní appalachian prostředí.
an epa review of arch coal’s proposed spruce 1 project in west virginia stated that the project could not be carried forward without adverse impacts to the surrounding appalachian environment.

poloha: nachází se pouhých 6 km od boone a appalachian státní kampus, hillwind... detaily a možnost objednání >>>
location: the relais alla... details and ordering >>>

začíná (končí) zde "appalachian trail" - která vede až do georgia a jejíž délka je 3 488 km.
the "appalachian trail" starts (ends) here and you can use it to hike as far as georgia. it's length is 2 162.2 miles.

going farther back in time, during the phanerozoic eon (going back over 500 million years) the major 'ice-house' periods (including glaciations and also periods with less but still significant ice, such as now (antarctica, greenland) correspond to periods with lower co2 (there had been some lack of correlation for the brief cold snap of the ordivician, but newer work suggests that a sufficient drawdown in co2 at that time could have or would have been caused by enhanced chemical weathering caused by the rise of the appalachian mountains).
going farther back in time, during the phanerozoic eon (going back over 500 million years) the major 'ice-house' periods (including glaciations and also periods with less but still significant ice, such as now (antarctica, greenland) correspond to periods with lower co2 (there had been some lack of correlation for the brief cold snap of the ordivician, but newer work suggests that a sufficient drawdown in co2 at that time could have or would have been caused by enhanced chemical weathering caused by the rise of the appalachian mountains).