• Aucun résultat trouvé

Rotation de figures à 5 sommets -- 2 étapes (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Rotation de figures à 5 sommets -- 2 étapes (A)"

Copied!
2
0
0

Texte intégral

(1)

Rotations (A)

Dessinez l’image finale et les ´etapes interm´ediaires de la rotation d´ecrite.

0

Rotation de 180

autour du point (1, 1).

Rotation de 180

autour du point (-4, -1).

-

x

6

y

`````````````````````````````````BBB B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B                                   @@ @@@

Rotation de 180

autour du point (5, -4).

Rotation dans le sens antihoraire de 90

autour

du point (1, 0).

-

x

6

y

S S S S S S S S S S S S S S S S S EEEE EEEE EEEE EEEE E SS SS SS SS S!!!!!!!!!!!!!!!!!!!!!

Rotation de 180

autour du point (3, 2).

Rotation de 180

autour du point (2, -1).

-

x

6

y

               Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z @ @ @ @ @ @ @ @ @ XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX

Rotation de 180

autour du point (-4, 2).

Rotation dans le sens antihoraire de 90

autour

du point (1, 4).

-

x

6

y

( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( (            @@ @@@ @@ @@ @@@ @@ @@ @    

MathsLibres.com

(2)

Rotations (A) Solutions

Dessinez l’image finale et les ´etapes interm´ediaires de la rotation d´ecrite.

0

Rotation de 180

autour du point (1, 1).

Rotation de 180

autour du point (-4, -1).

-

x

6

y

`````````````````````````````````BBB B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B                                   @@ @@@ ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` BB BB BBBB BBBB BBBB BBBB BB BBBB BBBB BBBB BBBB BBB    @ @ @ @ @ `````````````````````````````````BBB B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B B                                   @@ @@ @ x x

Rotation de 180

autour du point (5, -4).

Rotation dans le sens antihoraire de 90

autour

du point (1, 0).

-

x

6

y

S S S S S S S S S S S S S S S S S EEEE EEEE EEEE EEEE E SS SS SS SS S!!!!!!!!!!!!!!!!!!!!! SS SS SS SS SS SS SS SS S EEEE EE EE EE EE EE EE E S S S S S S S S S ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !     ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( (          LL LL LL LL LL LL LL LL LL LL L x x

Rotation de 180

autour du point (3, 2).

Rotation de 180

autour du point (2, -1).

-

x

6

y

               Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z @ @ @ @ @ @ @ @ @ XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX         ZZZ ZZ ZZ ZZ ZZ ZZ ZZZ ZZ ZZ ZZ ZZZ @@ @@ @@ @@ @ X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X                Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z Z @ @ @ @ @ @ @ @ @ XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX x x

Rotation de 180

autour du point (-4, 2).

Rotation dans le sens antihoraire de 90

autour

du point (1, 4).

-

x

6

y

( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( (            @@ @@@ @@ @@ @@@ @@ @@ @     (((((((((((((((((((((((((      @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @                  EE EE EE EE EE EE EE EE EE EE EE EE E ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ` ZZZ ZZZZZZZ ZZZZZZZ x x

MathsLibres.com

Références

Documents relatifs

Integration of landslide hazard maps into probabilistic risk assessment in context of global changes: an alpine test site... 1 Integration of landslide hazard maps into

Effects of depth, soil and vegetation types on indicators of soil organic carbon lability in forest soils.. Laure Soucémarianadin, Lauric Cécillon, Bertrand Guenet, Claire

The manner in which bubble nucleation occurred, with bubbles first nucleating after ~40°C of heating above the temperature at which the daughter minerals dissolved, followed

enlarged by wave disturbances and dissipated by the small ‐scale diffusion the differences between measurements and model output suggest that the de ficiencies in the modeled L e

Benthic foraminiferal δ 13 C, seawater carbonate ion concentration ([CO 3 2− ]) estimated from the Sr/Ca, and paleotemperature reconstructed on the basis of the Mg/Li of

In this paper, preliminary results comparing two preparation methods for dating bone are presented: a modified version of the Longin method and the ninhydrin protocol

The isotopic signature of this DIC can be rapidly transferred to the autotrophic OM pool of the river by photosynthesis of plankton and algae (Fontugne et al. In the Rhône River

The warming trend during 7 –2 ka BP recorded in the Chongce record (Figures 2a and 4a) is also observed in some of the Holocene temperature reconstructions, including the mean