• Aucun résultat trouvé

Addition de Coeurs Doux (A Un Chiffre) (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Addition de Coeurs Doux (A Un Chiffre) (A)"

Copied!
2
0
0

Texte intégral

(1)

Addition de Cœurs Doux (A)

Quelle est la valeur de chaque cœur doux?

3 +

i

= 8

m

+ 6 = 12 5 +

g

= 11

p

+ 8 = 11 8 +

h

= 17

n

+ 1 = 10 7 +

f

= 15

q

+ 7 = 12 2 +

e

= 8

t

+ 5 = 10 7 +

c

= 14

k

+ 2 = 5 4 +

j

= 10

l

+ 1 = 5 6 +

b

= 9

o

+ 3 = 8 3 +

d

= 11

s

+ 6 = 14 4 +

a

= 11

r

+ 8 = 14

(2)

Addition de Cœurs Doux (A) Réponses

Quelle est la valeur de chaque cœur doux?

3 + 5 = 8 6 + 6 = 12 5 + 6 = 11 3 + 8 = 11 8 + 9 = 17 9 + 1 = 10 7 + 8 = 15 5 + 7 = 12 2 + 6 = 8 5 + 5 = 10 7 + 7 = 14 3 + 2 = 5 4 + 6 = 10 4 + 1 = 5 6 + 3 = 9 5 + 3 = 8 3 + 8 = 11 8 + 6 = 14 4 + 7 = 11 6 + 8 = 14

Références

Documents relatifs

On entend également par « puiser dans vos connaissances littéraires » le fait de vous référer à d’autres œuvres que les textes proposés, de relier ces derniers à des courants

Figure 5 shows a two-layer structure of the SABL south of the Hoggar mountains, with a clean air layer (up to 1.5 km above ground level) advected from the east underneath a dust

By comparing the data of relative humidity, temperature and water vapor volume mixing ratio at two different heights (near-surface, ∼ 23 m above the surface), we demonstrate that

The ExoMars Atmospheric Mars Entry and Landing Investigation and Analysis (AMELIA) experiment in 2016 aimed to exploit the engineering data recorded during

H.: Global atmospheric effects of massive smoke injections from a nuclear war: Results from general circulation model simulations, Nature, 308, 21–25, 1984.

In contrast to many studies that adopt a de facto local view of land– atmosphere coupling (i.e., relating the land surface conditions and atmosphere at a particular point or

Variations of the slope M of the linear regression with the mean square root of age, (a) for the South Atlantic Ocean and (b) for the East Indian Ocean... Ridge height variations

the following picture: incident magnetosheath ULF waves (possibly generated near the bow shock) lead to enhanced fluctuation amplitudes at the magnetopause because of res-