• Aucun résultat trouvé

Transformation variées -- Figures à 4 sommets -- 3 étapes (A)

N/A
N/A
Info
Télécharger
Protected

Academic year: 2021

Partager "Transformation variées -- Figures à 4 sommets -- 3 étapes (A)"

Copied!
2
0
0

Chargement.... (Voir le texte intégral maintenant)

Texte intégral

(1)

Transformations G´eom´etriques (A)

Dessinez l’image finale et les ´etapes interm´ediaires des transformations d´ecrites.

0

D´eplacement de la figure par (-2, -4).

Rotation dans le sens horaire de 90◦ autour du point (-2, -3).

Homoth´etie de centre (-4, 2) et de rapport 3.

-

x

6

y

CCCC CCCC CCCC CCCC CCCC CCCC CCCC C H H H H H H H H H   

Homoth´etie de centre (-5, 3) et de rapport 13. D´eplacement de la figure par (1, 0).

Rotation dans le sens antihoraire de 90◦ autour du point (-5, 5). -

x

6

y

cc ccc cc ccc ccc cc ccc ccc cc cc              " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " "                 

Homoth´etie de centre (0, 5) et de rapport 4. D´eplacement de la figure par (2, 0).

Homoth´etie de centre (5, -3) et de rapport 2.

-

x

6

y

  lllll

D´eplacement de la figure par (3, 1). D´eplacement de la figure par (-2, 1). D´eplacement de la figure par (5, -3).

-

x

6

y

         h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h

MathsLibres.com

(2)

Transformations G´eom´etriques (A) Solutions

Dessinez l’image finale et les ´etapes interm´ediaires des transformations d´ecrites.

0

D´eplacement de la figure par (-2, -4).

Rotation dans le sens horaire de 90◦ autour du point (-2, -3).

Homoth´etie de centre (-4, 2) et de rapport 3.

-

x

6

y

CCCC CCCC CCCC CCCC CCCC CCCC CCCC C H H H H H H H H H    CCCC CC CCCC CCCC CCCC CCCC CCCC CCC H H H H H H H H H                                    XXXXXXXXX                                                                                                XXXXXXXXXXXXXXXXXXXXXXXXXXXXX x x

Homoth´etie de centre (-5, 3) et de rapport 13. D´eplacement de la figure par (1, 0).

Rotation dans le sens antihoraire de 90◦ autour du point (-5, 5). -

x

6

y

cc ccc cc ccc ccc cc ccc ccc cc cc              " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " "                  lllllllll      " " " " " " " " "       lllllllll      " " " " " " " " "       %%%% %%%%%JJJJJ TT TT TT TT T H H H H H H H H H H H H H H H H H x x

Homoth´etie de centre (0, 5) et de rapport 4. D´eplacement de la figure par (2, 0).

Homoth´etie de centre (5, -3) et de rapport 2.

-

x

6

y

  lllll          ccc cc cc ccc cc cc ccc cc cc          ccc cc cc ccc cc cc ccc cc cc                    ccc cc cc ccc cc cc cc cc cc cc cc cc ccc cc cc cc ccc cc c x x

D´eplacement de la figure par (3, 1). D´eplacement de la figure par (-2, 1). D´eplacement de la figure par (5, -3).

-

x

6

y

         h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h       h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h          h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h          h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h h

MathsLibres.com

Références

Télécharger maintenant ( PDF - 2 Page - 50.13 KB )

Documents relatifs

Micromechanics of brittle faulting and cataclastic flow in Alban Hills tuff

[68] In Figure 13 we replot our Alban Hills tuff data for C* in Figure 12, with the differential stress and mean stress at the onset of shear‐enhanced compaction normalized by

Exercices PDF / Lecture efficace / 4. Lire pour préparer un travail / 14. Journal de bord

Comme dans les autres formes de collecte de données, le lecteur s’efforce certes d’être objectif, mais l’écriture du journal de bord met surtout en évidence son apport person-

Forecasting volcanic eruptions and other material failure phenomena: an evaluation of the failure forecast method

On synthetic data the GLM method, assuming an error structure can be approximated by a Gaussian or Poissonian distribution, provides substantially higher quality (less biased and

Multifractal analysis of the pore space of real and simulated sedimentary rocks

Downloaded from https://academic.oup.com/gji/article/200/2/1108/607906 by Bibliothèque Universitaire de médecine - Nîmes user on 11 June 2021.. Giri et al. The open circles show

Effects of depth, soil and vegetation types on indicators of soil organic carbon lability in forest soils

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

Experimentally induced volumetric re-equilibration of plagioclase-hosted melt inclusions

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

Isotopic Signature (δ 13 C, ∆ 14 C) of DIC in Sediment Pore Waters: An Example from the Rhone River Delta

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

Temperature Trends in the Northwestern Tibetan Plateau Constrained by Ice Core Water Isotopes Over the Past 7,000 Years

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