CINEMANIA: Guess the movie title
[1485] CINEMANIA: Guess the movie title - Film was made in 2003. - #brainteasers #movie #film #cinemania - Correct Answers: 38 - The first user who solved this task is Sanja Šabović
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CINEMANIA: Guess the movie title

Film was made in 2003.
Correct answers: 38
The first user who solved this task is Sanja Šabović.
#brainteasers #movie #film #cinemania
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Rider

After a round of golf, four ladies sat around the club house, chatting.
Seeing the ladies, the Pro approached them and asked: "How did your game go?
The first lady, a brunette, said she had a good round ... making the comment that she actually had 25 riders. The Pro was a bit perplexed not knowing what a "Rider" was.
The second was a blonde lady who quickly chimed in and said that she had a very good round as well with 16 riders.
The third lady then said that her round was average and that she only had 10 riders.
The fourth lady admitted that she played the worst round of the day and that she only had 2 riders all day long.
The Pro was completely confused not knowing what the term "rider" meant. But, because he didn't want to look dumb, he made a quick polite remark, wished the ladies well and then left.
He then approached the bartender and asked "Hey, can you tell me what these ladies are talking about when they refer to "Riders"?"
The bartender simply smiled and said..."A 'Rider" is when you hit a shot long enough to ride on the golf cart to your ball.    

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Classification of geological eras

In 1759, Italian geologist Giovanni Arduino (1714-1795) dated a letter to Professor A.Vallisneri the younger, in which Arduino proposed a classification of Earth's surface rocks according to four brackets of successively younger orders: Primary, Secondary, Tertiary and Quaternary. These are the four geological eras used today. The volcanic rocks without fossils which he saw in the Atesine Alps that formed the cores of large mountains he called Primary. Overlying them, the fossil rich rocks of limestone and clay that were found on the prealpine flanks of the mountains he called Secondary. The less consolidated fossil-bearing rocks of the subalpine foothills, he named Tertiary, and the alluvial rock deposits in the plains were the Quaternary.«
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