Given a text passage, come up with an appropriate title for it. The title should accurately represent what the main focus of the passage is. The title of a passage may be present in the first few sentences of the passage and/or be referred to multiple times in the passage. The title should be 1-5 words long.

Example Input: Cheaper by the Dozen is a semi-autobiographical novel written by Frank Bunker Gilbreth , Jr. and Ernestine Gilbreth Carey , published in 1948 . The novel recounts the authors ' childhood lives growing up in a household of 12 kids . The bestselling book was later adapted into a feature film by Twentieth Century Fox in 1950 and followed up by the sequel , Belles on Their Toes ( 1950 ) , which was adapted as a 1952 film .
Example Output: Cheaper by the Dozen

Example Input: Night at the Museum is a 2006 American fantasy - comedy film directed by Shawn Levy and written by Robert Ben Garant and Thomas Lennon , based on the 1993 children 's book of the same name by Croatian illustrator Milan Trenc . The film stars Ben Stiller as Larry Daley , a divorced father who applies for a job as a night watchman at New York City 's American Museum of Natural History and subsequently discovers that the exhibits , animated by a magical Egyptian artifact , come to life at night .
Example Output: Night at the Museum

Example Input: Post-glacial rebound ( also called either isostatic rebound or crustal rebound ) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period , through a process known as isostatic depression . Post-glacial rebound and isostatic depression are different parts of a process known as either glacial isostasy , glacial isostatic adjustment , or glacioisostasy . Glacioisostasy is the solid Earth deformation associated with changes in ice mass distribution . The most obvious and direct effects of post-glacial rebound are readily apparent in parts of Northern Eurasia , Northern America , Patagonia , and Antarctica . However , through processes known as ocean siphoning and continental levering , the effects of post-glacial rebound on sea level are felt globally far from the locations of current and former ice sheets .
Example Output:
Post-glacial rebound