• Aucun résultat trouvé

Homothéties de figures à 3 sommets par rapport à l'origine -- 1er quadrant (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Homothéties de figures à 3 sommets par rapport à l'origine -- 1er quadrant (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, 0) et de rapport

1

3

.

-

x

6

y

# # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # #         

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

-

x

6

y

                         HHHHHHHHHHHHH

Homoth´etie de centre (0, 0) et de rapport

1

3

.

-

x

6

y

                             @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @

Homoth´etie de centre (0, 0) et de rapport 3.

-

x

6

y

HHHHHHHHH

(2)

L’Homoth´etie (A) Solutions

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

0

Homoth´etie de centre (0, 0) et de rapport

1

3

.

-

x

6

y

# # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # #          # # # # # # # # # # # # # # # # # # # # #  x

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

-

x

6

y

                         HHHHHHHHHHHHH                                                  HHHHHHHHHHHHHHHHHHHHHHHHH x

Homoth´etie de centre (0, 0) et de rapport

1

3

.

-

x

6

y

                             @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @          @ @ @ @ @ @ @ @ @ x

Homoth´etie de centre (0, 0) et de rapport 3.

-

x

6

y

HHHHHHHHH HHHHHHHHHHHHHHHHHHHHHHHHHHHHH x

MathsLibres.com

Références

Documents relatifs

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 open loop mean contrast degrades by a factor of four while the closed loop mean contrast remains at the initial value of 8.5 × 10 −8 within a standard deviation of 2.4 × 10 −8

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

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