martes, 2 de junio de 2009

¿Cuántas entradas has hecho?14 entradas
¿Cuántas entradas crees que debería haber por trimestre?Todas las que ha mandado la profesora
¿Cúal es la que más te ha gustado?los videos que hacemos sobre nosotros y la clase
¿Cúal la que menos?Redactar en ingles
¿Cúal ha sido la más difícil?el cuento de charlie boone
¿Fue fácil hacer el Blog?se podria decir que si
¿Habéis trabajado igual todos los miembros del grupo?si
¿Preferirías hacer un blog individual?no
¿Seguirás con el Blog el año que viene?si
¿Hay algún tema sobre lo que te gustaría trabajar el curso próximo?no
¿Cuál es el número ideal de personas para hacer el Blog?dos
¿Te gustaría que hubiera alguna entrada de tema libre?si
¿Has cambiado la plantilla o conservas la original?la e cambiado
¿Quieres hacer alguna sugerencia para el año que viene?que deje hacer redacciones sobre lo que cada uno quiera:grupo de musica,peliculas,libros....

jueves, 2 de abril de 2009

CHARLIE BONE BOOKS


Charlie bone a books

lunes, 30 de marzo de 2009

CHARLIE BONE

FIRST

Charlie Brown shows the optimistic side of the loneliness - as(like) in company of his(her,your) inseparable friends, beginning for 12-year-old Linus - and his(her,your) inseparable mantita-, a minor year that he(it), his(her,your) selfish minor sister 10-year-old Sally, his(her,your) overbearing companion 11-year-old Lucy, and his(her,your) other companions of baseball (there is remembered that he, as the rest of the equipment(team), is a terrible player) as the pianist Schroeder. In addition, and though there were feeling attraction for him(it) his(her,your) two friends Marcia and Patty (to the one that says always things mistaken in the wrong moment), he(it) was in love with a red-haired girl of long hair up to the shoulders called: 14-year-old Cindy. That never met portrayed in the comics and that was meditating from off, with that very rarely he(she) speaks.

SECOND

THIRD

Go away

The book we are going to read is "Midnight for Charlie Bone"





sábado, 14 de marzo de 2009

What I going to do this weekend

I going to visit my friend elisa.I am going watch tv with my friend elisa and celia;the sunday I am going to church with my parents and my brother. On Sunday evening I am going to study awhile and afterwards(later) it will be able only with my friends to give a walk and in the night vere my favorite series and the 11 11:30 me ire to the bed.On Monday morning I am going to go to class of 8:30 to 2:30 afterwards(later) comere and later I am going to study with my cousin and at 7:30 I am going to go to classes of mathematics.

martes, 10 de marzo de 2009

martes, 3 de febrero de 2009

Hello,I am Bea. I am 13 years old,I have got bormw hear,my brother is Sergio my mather is Elena and my father is Manuel.
I am Paula I am 13 years old ,I am tall and thin ,I have got bromw hear in my family are 5 person,my sister is Carmen , my brother is Daniel , my father is Salvador and my mather is Carmen.
we are going at the high school Rio Duero.
we hate play the basketball
we love the beatiful boys and the music.
we are the friends forever.




martes, 20 de enero de 2009

Naturally occurring earthquakes

Tectonic earthquakes will occur anywhere within the earth where there is sufficient stored elastic strain energy to drive fracture propagation along a fault plane. In the case of transform or convergent type plate boundaries, which form the largest fault surfaces on earth, they will move past each other smoothly and aseismically only if there are no irregularities or asperities along the boundary that increase the frictional resistance. Most boundaries do have such asperities and this leads to a form of stick-slip behaviour. Once the boundary has locked, continued relative motion between the plates leads to increasing stress and therefore, stored strain energy in the volume around the fault surface. This continues until the stress has risen sufficiently to break through the asperity, suddenly allowing sliding over the locked portion of the fault, releasing the stored energy. This energy is released as a combination of radiated elastic strain seismic waves, frictional heating of the fault surface, and cracking of the rock, thus causing an earthquake. This process of gradual build-up of strain and stress punctuated by occasional sudden earthquake failure is referred to as the Elastic-rebound theory

martes, 13 de enero de 2009

New Year Resolutions

Paula:
I am going to study more
I am going to go shopping
I am going to meet whit my friends
I am going to learn lessons
I am going to eat vegetables

Beatriz:
I am going to study very good.
I am going to listen to my brother
I am going to read more
I am going to help to my mather
I am going to go shopping.