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Bueno permitidme por única vez hablar en castellano en este hilo.

Abro dicho hilo para que hablemos en Inglés, pongamos preguntas o contemos lo que queramos, y para las que sepan más pues que nos corrijan a las que sabemos menos y esas cosas, también si conoceis cuentos o historias cortitas las poneis...todo lo que se os ocurra Wink

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Hello, little girls! Today, this morning I went to Bodybell and saw the new collection of Essence, is very beautiful but I didn´t buy nothing becouse I have thousand things and I can´t spend more money. And you, what did you do today?
Hello!

I thing it's a good idea! these days I was thinking on doing something like this to practise my English.

I'm planing to do some exercise buy I'm too but in all kind of sports, what do you recommend me to do?
Thank you!!
If you are referring to that kind of sport to practice I would recommend you swim becouse now begin the cold and running is harder than going to the swimming pool, the water almost massage your skin, is a very good sport
The other option is to go to de gym
Hello girls!

How are you?

I thik that today isn´t the best day of my life. I am very sad...
Why are you sad Sasha_Fierce? You have to be happy, we are here for anything that you need!!!

kisses!!!
Thank you Bolboreta!
Hello!
I have not seen this post, I think it's perfect to learn more English.

Good idea bolboreta!.
At the moment I dont speak english very well. I´ts a very good idea to practice!
Don´t mind!!! this is for practice and we sure make a lot of mistakes but don´t worry be happy xDDD

kisses!!!
Awww I love english, I wish I could learn it but the best way to do it it's by here (thanks bolboreta) and with movies using subtitles, and listening songs too!!


xoxo (more english) lol
What is the last film that you have seen? Did you like it? tell us
(11-11-2010 23:45 PM)Yoli Escribió: [ -> ]Awww I love english, I wish I could learn it but the best way to do it it's by here (thanks bolboreta) and with movies using subtitles, and listening songs too!!


xoxo (more english) lol

I also see films with subtitles and now I am seeing Lost in English with my brother. Is the second time that I see Lost Risax But the first time I saw it in spanish
Zipy
Awww Lost, my favourite tv show, i was in love with Boone Smile I cried a lot when it ended.

I saw the last episodies in english becouse i couldn't wait to see it in spanish (THANKS GOD FOR GIVE US INTERNET)

And now like a good girl I have to sleep. Good nigth and sweet dreams Smile

xoxo
What are you doing this weekend?

I don´t know yet, but I will go of shopping if I can
I'll go shoppint tomorrow (if I can), I wanna buy a shoes I saw last week
I think that today i am going to dinner in a restaurant... I don´t know...
Hi everyone,I love Sunday but I can do what I do not make the rest of the week, I take to all the day seeing makeups videos in youtube, soon Im going yo house of my mother to eat, the eat of my moon is the best of the world,when you do not live with her is sorprised, oh my god is 13.44 I must dress me already, see you later bye
Hello girls!

I hope that your weekend had been very good, tomorrow we begin a new week and each day we are more near to Christmas days, when will you put the tree and the decoration? I don´t know yet .
(14-11-2010 13:45 PM)aidy85 Escribió: [ -> ]Hi everyone,I love Sunday but I can do what I do not make the rest of the week, I take to all the day seeing makeups videos in youtube, soon Im going yo house of my mother to eat, the eat of my moon is the best of the world,when you do not live with her is sorprised, oh my god is 13.44 I must dress me already, see you later bye

es mum aidy moon es luna Juas Big Grin
jajaja Speaking of the moon I give you a little information Wink in English of course:

The Moon is the only natural satellite of Earth:

Called Luna by the Romans, Selene and Artemis by the Greeks, and many other names in other mythologies.


The Moon, of course, has been known since prehistoric times. It is the second brightest object in the sky after the Sun. As the Moon orbits around the Earth once per month, the angle between the Earth, the Moon and the Sun changes; we see this as the cycle of the Moon's phases. The time between successive new moons is 29.5 days (709 hours), slightly different from the Moon's orbital period (measured against the stars) since the Earth moves a significant distance in its orbit around the Sun in that time.

Due to its size and composition, the Moon is sometimes classified as a terrestrial "planet" along with Mercury, Venus, Earth and Mars.

[Imagen: foot.jpg]

The Moon was first visited by the Soviet spacecraft Luna 2 in 1959. It is the only extraterrestrial body to have been visited by humans. The first landing was on July 20, 1969 (do you remember where you were?); the last was in December 1972. The Moon is also the only body from which samples have been returned to Earth. In the summer of 1994, the Moon was very extensively mapped by the little spacecraft Clementine and again in 1999 by Lunar Prospector.


[Imagen: earthmo2.jpg]

The gravitational forces between the Earth and the Moon cause some interesting effects. The most obvious is the tides. The Moon's gravitational attraction is stronger on the side of the Earth nearest to the Moon and weaker on the opposite side. Since the Earth, and particularly the oceans, is not perfectly rigid it is stretched out along the line toward the Moon. From our perspective on the Earth's surface we see two small bulges, one in the direction of the Moon and one directly opposite. The effect is much stronger in the ocean water than in the solid crust so the water bulges are higher. And because the Earth rotates much faster than the Moon moves in its orbit, the bulges move around the Earth about once a day giving two high tides per day. (This is a greatly simplified model; actual tides, especially near the coasts, are much more complicated.)

But the Earth is not completely fluid, either. The Earth's rotation carries the Earth's bulges slightly ahead of the point directly beneath the Moon. This means that the force between the Earth and the Moon is not exactly along the line between their centers producing a torque on the Earth and an accelerating force on the Moon. This causes a net transfer of rotational energy from the Earth to the Moon, slowing down the Earth's rotation by about 1.5 milliseconds/century and raising the Moon into a higher orbit by about 3.8 centimeters per year. (The opposite effect happens to satellites with unusual orbits such as Phobos and Triton).

The asymmetric nature of this gravitational interaction is also responsible for the fact that the Moon rotates synchronously, i.e. it is locked in phase with its orbit so that the same side is always facing toward the Earth. Just as the Earth's rotation is now being slowed by the Moon's influence so in the distant past the Moon's rotation was slowed by the action of the Earth, but in that case the effect was much stronger. When the Moon's rotation rate was slowed to match its orbital period (such that the bulge always faced toward the Earth) there was no longer an off-center torque on the Moon and a stable situation was achieved. The same thing has happened to most of the other satellites in the solar system. Eventually, the Earth's rotation will be slowed to match the Moon's period, too, as is the case with Pluto and

[Imagen: farside.jpg]

Actually, the Moon appears to wobble a bit (due to its slightly non-circular orbit) so that a few degrees of the far side can be seen from time to time, but the majority of the far side (left) was completely unknown until the Soviet spacecraft Luna 3 photographed it in 1959. (Note: there is no "dark side" of the Moon; all parts of the Moon get sunlight half the time (except for a few deep craters near the poles). Some uses of the term "dark side" in the past may have referred to the far side as "dark" in the sense of "unknown" (eg "darkest Africa") but even that meaning is no longer valid today!)

The Moon has no atmosphere. But evidence from Clementine suggested that there may be water ice in some deep craters near the Moon's south pole which are permanently shaded. This has now been reinforced by data from Lunar Prospector. There is apparently ice at the north pole as well.

The Moon's crust averages 68 km thick and varies from essentially 0 under Mare Crisium to 107 km north of the crater Korolev on the lunar far side. Below the crust is a mantle and probably a small core (roughly 340 km radius and 2% of the Moon's mass). Unlike the Earth, however, the Moon's interior is no longer active. Curiously, the Moon's center of mass is offset from its geometric center by about 2 km in the direction toward the Earth. Also, the crust is thinner on the near side.

There are two primary types of terrain on the Moon: the heavily cratered and very old highlands and the relatively smooth and younger maria. The maria (which comprise about 16% of the Moon's surface) are huge impact craters that were later flooded by molten lava. Most of the surface is covered with regolith, a mixture of fine dust and rocky debris produced by meteor impacts. For some unknown reason, the maria are concentrated on the near side.


[Imagen: galmoon.jpg]

Most of the craters on the near side are named for famous figures in the history of science such as Tycho, Copernicus, and Ptolemaeus. Features on the far side have more modern references such as Apollo, Gagarin and Korolev (with a distinctly Russian bias since the first images were obtained by Luna 3). In addition to the familiar features on the near side, the Moon also has the huge craters South Pole-Aitken on the far side which is 2250 km in diameter and 12 km deep making it the the largest impact basin in the solar system and Orientale on the western limb (as seen from Earth; in the center of the image at left) which is a splendid example of a multi-ring crater.

A total of 382 kg of rock samples were returned to the Earth by the Apollo and Luna programs. These provide most of our detailed knowledge of the Moon. They are particularly valuable in that they can be dated. Even today, more than 30 years after the last Moon landing, scientists still study these precious samples.

Most rocks on the surface of the Moon seem to be between 4.6 and 3 billion years old. This is a fortuitous match with the oldest terrestrial rocks which are rarely more than 3 billion years old. Thus the Moon provides evidence about the early history of the Solar System not available on the Earth.

Prior to the study of the Apollo samples, there was no consensus about the origin of the Moon. There were [/align]: co-accretion which asserted that the Moon and the Earth formed at the same time from the Solar Nebula; fission which asserted that the Moon split off of the Earth; and capture which held that the Moon formed elsewhere and was subsequently captured by the Earth. None of these work very well. But the new and detailed information from the Moon rocks led to the impact theory: that the Earth collided with a very large object (as big as Mars or more) and that the Moon formed from the ejected material. There are still details to be worked out, but the impact theory is now widely accepted.

The Moon has no global magnetic field. But some of its surface rocks exhibit remanent magnetism indicating that there may have been a global magnetic field early in the Moon's history.

With no atmosphere and no magnetic field, the Moon's surface is exposed directly to the solar wind. Over its 4 billion year lifetime many ions from the solar wind have become embedded in the Moon's regolith. Thus samples of regolith returned by the Apollo missions proved valuable in studies of the solar wind.


Read more about The Moon l Phases, Orbit and distance from the Earth by nineplanets.org

VOCABULARY:

tides: mareas
weaker: débil
bulge: protuberancia, bulto
crust: corteza
beneath: abajo, debajo
i.e. : viene del latín "it est"= this is, esto es
wobble: temblar
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