Mandy her friends for dinner at eight o’clock
B

A will have met
B will have been meeting
C is meeting D meets

2 Jack hopes he a famous inventor one day.
A will be becoming C will become
B will have become D is becoming
3 They’ve bought tickets and they the science fair.

A are going to visit
B will have visited
C are visiting D visit

4 This time next Friday they to Mexico in order to attend the sailing competition.
A will be travelling C are travelling
B travel D will travel
5 Even though they were covered in chocolate, James was reluctant the insects.
A eating B toeat C eat D eats

6 By the end of the month, I at the science centre for four years.
A will have been working
B am going to work
C am working D will work

7 The Insect Restaurant at 11 pm on weekdays.
A will have been closing C is closing
B will have closed D closes
8 In order to avoid yourself while skating, you should wear protective clothing.
A injures C to injure
B injure D injuring

9 Let’s go to the festival at 6 pm; I work by then.
A will have been finishing B will have finished
C am finishing D finish

10 He can’t in the skiing tournament next week because he’s sprained his ankle.
A competing C compete
B competes D to compete

11 Watch out! Those rocks on you!
A will fall C are falling
B are going to fall D will be fal

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макс17281

Английский язык

4,7(83 оценок)

Earthquake - it tremors and vibrations of the earth's surface, which arise as a result of sudden shifts and breaks in the crust or upper mantle and transmitted over long distances in the form of elastic vibrations. the intensity of the earthquake is estimated at seismic scores. known two major seismic belt of the earth: the pacific, which covers the ring of the pacific ocean, and the mediterranean, which stretches across eurasia south of the iberian peninsula in the west to the east of the malay archipelago. within oceans significant seismic activity sredneokeanicheskie different ranges. the most famous earthquake of lisbon (1755), california (1906), messinian (1908), ashgabat (1948), chilean (1960), armenian (1988), iran (1990 g earthquakes are among the most destructive natural forces. the most powerful earthquake could be 10 thousand times more powerful than the atomic bomb dropped on hiroshima in 1945. strong earthquakes are catastrophic, second in the number of victims of typhoons and only ten times getting over the eruption of volcanoes. material damage to a devastating earthquake could reach hundreds of millions of dollars. number of weak earthquakes is much more than the strong. thus, hundreds of thousands of earthquakes that occur each year on earth, only a few disastrous. they release about 1020 j of potential seismic energy, which represents only 0.01% of the heat energy of the earth, which is radiated into space. spatial distribution of earthquakes uneven. it is determined by the movement and interaction of lithospheric plates. the main seismic belt, which is allocated to 80% of the seismic energy is located in the pacific ocean near the trenches, where the promotion of young lithospheric plates beneath the continent. energy release notes in the eurasian fold belt in place of the collision of the eurasian plate with indian and african plates and areas sredneokeanicheskih ranges in terms of stretching the lithosphere. cells earthquakes are located at depths of up to 700 km, but the majority (3/4) of the seismic energy released in cells that are found at a depth of 70 km. the position of the earthquake source and place the beginning of mass transfer (hypocenter) determined by recording the seismic waves that occur during earthquakes (from weak earthquakes cell hypocenter and the same).