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» christie ally to plead guilty in new jersey bridge scandal (new york times)
» christie ally to plead guilty in new jersey bridge scandal (new york times)

* william h. gerdts, painting and sculpture in new jersey (princeton, nj: van nostrand, 1964), p. 56.
* william h. gerdts, painting and sculpture in new jersey (princeton, nj: van nostrand, 1964), p. 56.

huntsman formally entered the race for the republican presidential nomination on june 21, 2011, announcing his bid in a speech at liberty state park in new jersey, with the statue of liberty in the background—the same site where ronald reagan launched his campaign in 1980.
huntsman formally entered the race for the republican presidential nomination on june 21, 2011, announcing his bid in a speech at liberty state park in new jersey, with the statue of liberty in the background—the same site where ronald reagan launched his campaign in 1980.

" this position apparently precipitated a similar shift in emphasis at the cop 8 climate talks in new delhi several months later, "the shift satisfies the bush administration, which has fought to avoid mandatory cuts in emissions for fear it would harm the economy.
this position apparently precipitated a similar shift in emphasis at the cop 8 climate talks in new delhi several months later, "the shift satisfies the bush administration, which has fought to avoid mandatory cuts in emissions for fear it would harm the economy.

153. mars' atmosphere was probably never thick enough to keep temperatures on the planet's surface above freezing for the long term, suggests research published today in nature geoscience. although the planet's topography indicates that liquid water has flooded mars in the distant past, evidence increasingly suggests that those episodes reflect occasional warm spells, not a consistently hospitable phase of the planet's history. signs of flowing water on mars include layered sediments presumed to have been laid down in ancient lakes, as well as rugged canyons and lowlands apparently sculpted by massive floods. these had once prompted researchers to suggest that the red planet, now frigid and dry, was warm and wet throughout its early history, but that would have required an atmosphere much thicker than today's, a prospect that now seems unlikely, says edwin kite, a planetary scientist at princeton university in new jersey. ( www.nature.com ) in contrast to its cold past, mars is currently ina relatively temperate period, researchers think. b. the research indicates that floods on mars occurred only intermittently rather than during a long continuous period. c. floods were partly responsible for the canyons and lowlands existing on mars. d. mars' atmosphere has very rarely been such as to keep water above its freezing temperature.
153. mars' atmosphere was probably never thick enough to keep temperatures on the planet's surface above freezing for the long term, suggests research published today in nature geoscience. although the planet's topography indicates that liquid water has flooded mars in the distant past, evidence increasingly suggests that those episodes reflect occasional warm spells, not a consistently hospitable phase of the planet's history. signs of flowing water on mars include layered sediments presumed to have been laid down in ancient lakes, as well as rugged canyons and lowlands apparently sculpted by massive floods. these had once prompted researchers to suggest that the red planet, now frigid and dry, was warm and wet throughout its early history, but that would have required an atmosphere much thicker than today's, a prospect that now seems unlikely, says edwin kite, a planetary scientist at princeton university in new jersey. ( www.nature.com ) in contrast to its cold past, mars is currently ina relatively temperate period, researchers think. b. the research indicates that floods on mars occurred only intermittently rather than during a long continuous period. c. floods were partly responsible for the canyons and lowlands existing on mars. d. mars' atmosphere has very rarely been such as to keep water above its freezing temperature.