• Aucun résultat trouvé

Homothéties de figures à 3 sommets (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Homothéties de figures à 3 sommets (A)"

Copied!
2
0
0

Texte intégral

(1)

L’Homoth´etie (A)

Dessinez l’image de l’homoth´etie d´ecrite.

0

Homoth´etie de centre (0, -1) et de rapport 2.

-

x

6

y

JJ JJ JJ JJ JJ JJ JJ JJ Jaaa a a a a a a a a a a a a a a a a a a a a a a a a a a

Homoth´etie de centre (-5, -4) et de rapport

1

4

.

-

x

6

y

                                                                                                   H H H H H H H H H H H H H

Homoth´etie de centre (5, -1) et de rapport 2.

-

x

6

y

 

Homoth´etie de centre (5, -5) et de rapport 3.

-

x

6

y

     AAAAA

MathsLibres.com

(2)

L’Homoth´etie (A) Solutions

Dessinez l’image de l’homoth´etie d´ecrite.

0

Homoth´etie de centre (0, -1) et de rapport 2.

-

x

6

y

JJ JJ JJ JJ JJ JJ JJ JJ Jaaa a a a a a a a a a a a a a a a a a a a a a a a a a a JJ JJ JJ JJ JJ JJ JJ JJ JJ JJ JJ JJ JJ JJ JJ JJ JJ JJ Jaaa a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a a x

Homoth´etie de centre (-5, -4) et de rapport

1

4

.

-

x

6

y

                                                                                                   H H H H H H H H H H H H H                       x

Homoth´etie de centre (5, -1) et de rapport 2.

-

x

6

y

    x

Homoth´etie de centre (5, -5) et de rapport 3.

-

x

6

y

     AAAAA                  AA AA AA AA AA AA AA AA A x

MathsLibres.com

Références

Documents relatifs

In each region, Δsoc cropland minus initial natveg was calculated as the difference of soil carbon stocks densities of grid cells dominated by cropland grid cells with a

Combined with model-based design and automatic code generation, the potential of static analysis tools is increased greatly: More strict specification and development

Additionally, model results obtained with detailed aerosol microphysics are compared to those based on an aerosol bulk mass approach revealing the impact of dry deposition fluxes

The Central Indian Ocean recorded sev- eral major tectonic events: (i) parts of the basins were affected by the passage of two major hot spots, the Réunion and Kerguelen hot

Principal component analyses performed on individual S-FTIR hyperspectral images were strongly influenced by the dominant phase of the imaged area, either of mineral (for Areas 2

Our analysis shows that the poroelastic response to ocean tidal loading is controlled by the permeability structure of extrusive layer 2A, which varies considerably across sites

(a) Orthorectified mosaic obtained by projecting DISR images using the positions and orientations from the SPICE kernels only, (b) orthorectified mosaic obtained from the po- sition

High temperature impact melt breccias from the Rochechouart (France) meteorite crater record a magnetization component with antipodal, normal and reverse polarities.. The