• Aucun résultat trouvé

Compte de petites collections de sous US (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Compte de petites collections de sous US (A)"

Copied!
2
0
0

Texte intégral

(1)

Compte de Pi`eces de Monnaie (A)

Quelle est la valeur totale de chaque collection de pi`eces de monnaie?

1.

=

? 2.

=

? 3.

=

? 4.

=

? 5.

=

? 6.

=

? 7.

=

? 8.

=

?

Images de pi`eces de monnaie provenantes de la Monnaie des ´Etats-Unis

(2)

Compte de Pi`eces de Monnaie (A) Solutions

Quelle est la valeur totale de chaque collection de pi`eces de monnaie?

1.

=

$0.67

2.

=

$0.94

3.

=

$0.88

4.

=

$0.89

5.

=

$0.77

6.

=

$0.74

7.

=

$0.71

8.

=

$0.57

Images de pi`eces de monnaie provenantes de la Monnaie des ´Etats-Unis

Références

Documents relatifs

To confirm that this remains the case for the entire density range considered here, we show in Table 1 the results obtained for the internal energy and pressure at rep-

Character- istics of colored dissolved organic matter (CDOM) in the Western Arctic Ocean: relationships with microbial activities... The

The long-dashed line is for the case with high water vapor (9000 ppm) and a layer of smoke in- troduced to reduce the photolysis rates in the model. The ambient NO x in all

This concludes in a major improvement in using pypher ker- nels with e ffective PSFs with respect to Gaussian, circular or ADGS11 kernels from an image processing standpoint.. Next

We demonstrate that, from the optical to the near-infrared (IR) band, the polarized spectrum of NGC 4151 shows a much bluer power-law spectral index than that of the total

1.A greater understanding of how marine systems are affected by ocean acidification and warming is required through setting up long-term, basin scale monitoring

The sensitivity of the mean climatological diurnal amplitude of the surface temperature and that of the daily mean surface temperature to the soil thermal inertia were expressed as

The central and northern parts of the Bre´zouard and Thannenkirch granites character- ized by the feeble magmatic fabrics exhibit a weakly dominant NW-SE trending magnetic