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Mice21 [21]
3 years ago
8

In which sentence are the pronoun and antecedent not in agreement?

English
2 answers:
Grace [21]3 years ago
5 0

The correct answer is B. If the bus is late, he will be late to class.

Explanation:

In grammar, a pronoun is a word that replaces a noun for example she, he, it we; additionally, in sentences it is common these type of words replace a previous noun which is referred as antecedent and for this to be grammatically correct both the antecedent and the pronoun need to agree in gender and number. This implies if the noun presented is "Joseph" which is masculine and singular this can only be replaced by the noun "he" which is also masculine and singular or in the case the noun is "dog" this can be replaced by the pronoun "it".

Considering this, the sentence in which there is not an agreement between the pronoun and the antecedent is "If the bus is late, he will be late to class" because in this, the antecedent is "bus" and this should be replaced by the pronoun "it" that describes animals or objects but instead it has been replaced by "he" which refers to a person.

777dan777 [17]3 years ago
3 0
If the bus is late, he will be late to class.
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On 22 February 2011, at 12:51 pm (lunchtime), Christchurch was struck by a magnitude 6.3 earthquake. The quake was centred 10km south-east of the city at a depth of 5km. 185 people died, 164 people were seriously injured and there was major, widespread damage.

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On 22 February 2011, at 12:51 pm, Christchurch was struck by a magnitude 6.3 earthquake. The quake was centred 10km south-east of the city at a depth of 5km. In the ten minutes after it hit, there were 10 aftershocks of magnitude 4 or more.

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As had happened after the 4 September 2010 quake, there was a lot of liquefaction. Liquefaction happens when underground water in the soil comes to the surface. Thick muddy slush spreads everywhere, causing buildings and other structures to sink into the ground. Many roads, footpaths, schools and houses were flooded with silt.

There was a lot of confusion and panic, especially in the centre of the city. People were desperately trying to contact their friends and families, and to get back home. The phone lines and roads almost immediately became jammed.

Right after the earthquake, a lot of people left Christchurch. Small towns in the South Island welcomed many people from Christchurch. School kids were allowed to go to the schools at the places they were staying. Many people left for only a short while, but others chose to leave for good.

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185 people died and many thousands were injured as a result of the earthquake. 164 people were seriously injured.

Most of the victims were killed in two large building collapses: 115 people died when the six-storey Canterbury Television (CTV) building in Madras Street collapsed, and 18 people died when the 4-storey Pyne Gould Corporation (PGC) building in Cambridge Terrace collapsed. Rescue crews worked around the clock at both locations to dig out trapped people.

169 people died in the Central City and 16 people died in other parts of Christchurch.

Rescue crews from all over the world came to help. There were crews from Japan, the United States, the United Kingdom, Taiwan, Australia and other countries.

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The earthquake had a magnitude of 6.3 on the Richter scale. It was felt all over the South Island and in the lower part of the North Island.

The fault that caused the quake cannot be seen from the surface, but it runs about 6 km south of the city centre. Land around the fault, in the Port Hills, in Cashmere and in the seaside suburbs, rose, fell and slid.

Even though the February 2011 earthquake was smaller in magnitude than the September 2010 earthquake, its impact was much greater. The September earthquake happened at night, when most people were at home asleep. This meant that even though some large buildings collapsed, few people were nearby them when they were damaged. The February earthquake was also much more disastrous because there was a very high ‘ground acceleration’. Ground acceleration measures how much and how fast the ground (and things on it like buildings and natural features) moves during an earthquake. Some of the reasons why ground acceleration was so high in the February earthquake were the large amount of energy that the fault line released, the way the land under Christchurch was formed and how near Christchurch was to the fault. Also, the February earthquake was much shallower (closer to the surface) than the September one and it was closer to the city.

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