List Of Hallmark Hall Of Fame Episodes
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List Of Hallmark Hall Of Fame Episodes
The following is a list of episodes of the American television anthology series, ''Hallmark Hall of Fame''. *(v) indicates the production is available on videocassette. *(DVD) indicates the movie is available on DVD Seasons Season 1 (1951–52) Season 2 (1952–53) Season 3 (1953–54) Season 4 (1954–55) Season 5 (1955–56) Season 6 (1956–57) Season 7 (1957–58) Season 8 (1958–59) Season 9 (1959–60) Season 10 (1960–61) Season 11 (1961–62) Season 12 (1962–63) Season 13 (1963–64) Season 14 (1964–65) Season 15 (1965–66) Season 16 (1966–67) Season 17 (1967–68) Season 18 (1968–69) Season 19 (1969–70) Season 20 (1970–71) Season 21 (1971–72) Season 22 (1972–73) Season 23 (1973–74) Season 24 (1974–75) Season 25 (1975–76) Season 26 (1976–77) Season 27 (1977–78) :NOTE: Hallmark's #128 was "Peter Pan", a rerun of #121. The date and season ...
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Anthology Series
An anthology series is a radio, television, video game or film series that spans different genres and presents a different story and a different set of characters in each different episode, season, segment, or short. These usually have a different cast in each episode, but several series in the past, such as ''Four Star Playhouse'', employed a permanent troupe of character actors who would appear in a different drama each week. Some anthology series, such as '' Studio One'', began on radio and then expanded to television. Etymology The word comes from Ancient Greek ἀνθολογία (''anthología'', “flower-gathering”), from ἀνθολογέω (''anthologéō'', "I gather flowers"), from ἄνθος (''ánthos'', "flower") + λέγω (''légō'', "I gather, pick up, collect"), coined by Meleager of Gadara circa 60 BCE, originally as Στέφανος (στέφανος (''stéphanos'', "garland")) to describe a collection of poetry, later retitled anthology – see Gr ...
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Season 16 (1966–67)
A season is a division of the year based on changes in weather, ecology, and the number of daylight hours in a given region. On Earth, seasons are the result of the axial parallelism of Earth's tilted orbit around the Sun. In temperate and polar regions, the seasons are marked by changes in the intensity of sunlight that reaches the Earth's surface, variations of which may cause animals to undergo hibernation or to migrate, and plants to be dormant. Various cultures define the number and nature of seasons based on regional variations, and as such there are a number of both modern and historical cultures whose number of seasons varies. The Northern Hemisphere experiences most direct sunlight during May, June, and July, as the hemisphere faces the Sun. The same is true of the Southern Hemisphere in November, December, and January. It is Earth's axial tilt that causes the Sun to be higher in the sky during the summer months, which increases the solar flux. However, due to seasona ...
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Season 29 (1979–80)
A season is a division of the year based on changes in weather, ecology, and the number of daylight hours in a given region. On Earth, seasons are the result of the axial parallelism of Earth's tilted orbit around the Sun. In temperate and polar regions, the seasons are marked by changes in the intensity of sunlight that reaches the Earth's surface, variations of which may cause animals to undergo hibernation or to migrate, and plants to be dormant. Various cultures define the number and nature of seasons based on regional variations, and as such there are a number of both modern and historical cultures whose number of seasons varies. The Northern Hemisphere experiences most direct sunlight during May, June, and July, as the hemisphere faces the Sun. The same is true of the Southern Hemisphere in November, December, and January. It is Earth's axial tilt that causes the Sun to be higher in the sky during the summer months, which increases the solar flux. However, due to seasona ...
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Season 28 (1978–79)
A season is a division of the year based on changes in weather, ecology, and the number of daylight hours in a given region. On Earth, seasons are the result of the axial parallelism of Earth's tilted orbit around the Sun. In temperate and polar regions, the seasons are marked by changes in the intensity of sunlight that reaches the Earth's surface, variations of which may cause animals to undergo hibernation or to migrate, and plants to be dormant. Various cultures define the number and nature of seasons based on regional variations, and as such there are a number of both modern and historical cultures whose number of seasons varies. The Northern Hemisphere experiences most direct sunlight during May, June, and July, as the hemisphere faces the Sun. The same is true of the Southern Hemisphere in November, December, and January. It is Earth's axial tilt that causes the Sun to be higher in the sky during the summer months, which increases the solar flux. However, due to seasona ...
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Season 27 (1977–78)
A season is a division of the year based on changes in weather, ecology, and the number of daylight hours in a given region. On Earth, seasons are the result of the axial parallelism of Earth's tilted orbit around the Sun. In temperate and polar regions, the seasons are marked by changes in the intensity of sunlight that reaches the Earth's surface, variations of which may cause animals to undergo hibernation or to migrate, and plants to be dormant. Various cultures define the number and nature of seasons based on regional variations, and as such there are a number of both modern and historical cultures whose number of seasons varies. The Northern Hemisphere experiences most direct sunlight during May, June, and July, as the hemisphere faces the Sun. The same is true of the Southern Hemisphere in November, December, and January. It is Earth's axial tilt that causes the Sun to be higher in the sky during the summer months, which increases the solar flux. However, due to se ...
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Season 26 (1976–77)
A season is a division of the year based on changes in weather, ecology, and the number of daylight hours in a given region. On Earth, seasons are the result of the axial parallelism of Earth's tilted orbit around the Sun. In temperate and polar regions, the seasons are marked by changes in the intensity of sunlight that reaches the Earth's surface, variations of which may cause animals to undergo hibernation or to migrate, and plants to be dormant. Various cultures define the number and nature of seasons based on regional variations, and as such there are a number of both modern and historical cultures whose number of seasons varies. The Northern Hemisphere experiences most direct sunlight during May, June, and July, as the hemisphere faces the Sun. The same is true of the Southern Hemisphere in November, December, and January. It is Earth's axial tilt that causes the Sun to be higher in the sky during the summer months, which increases the solar flux. However, due to seasona ...
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Season 25 (1975–76)
A season is a division of the year based on changes in weather, ecology, and the number of daylight hours in a given region. On Earth, seasons are the result of the axial parallelism of Earth's axial tilt, tilted orbit around the Sun. In temperate and polar regions, the seasons are marked by changes in the intensity of sunlight that reaches the Earth's surface, variations of which may cause animals to undergo hibernation or to Migration (ecology), migrate, and plants to be dormant. Various cultures define the number and nature of seasons based on regional variations, and as such there are a number of both modern and historical cultures whose number of seasons varies. The Northern Hemisphere experiences most direct sunlight during May, June, and July, as the hemisphere faces the Sun. The same is true of the Southern Hemisphere in November, December, and January. It is Earth's axial tilt that causes the Sun to be higher in the sky during the summer months, which increases the solar ...
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