Seasons and how the Sun work on a Level Earth Gleasons Map

🌍 In the context of the Gleason's Map, which represents a specific flat Earth model, the description of seasons and the movement of the Sun differs significantly from the widely accepted heliocentric model.

🌞 Seasons on a Level Earth (Gleason's Map):
On the Gleason's Map, which portrays the Earth as a flat, level surface, the concept of seasons is explained in a way that differs from the well-established heliocentric model. According to this model:

☀️ Sun's Motion:
In the Gleason's Map model, the Sun is believed to move in a circular path above the flat Earth. This path creates a constant cycle of day and night, with the Sun rising in the east and setting in the west.

🔄 Changing Altitude:
To account for seasonal variations, it is proposed that the Sun also changes its altitude throughout the year. In this model, during the northern hemisphere's summer, the Sun is said to move closer to the center of the flat Earth, resulting in longer days and warmer temperatures. Conversely, during the northern hemisphere's winter, the Sun is positioned farther away from the center, leading to shorter days and cooler temperatures.

🌐 Equator and Tropics:
The Gleason's Map model suggests that the equator remains the warmest region year-round because it is closest to the Sun's path and maintains a high Sun angle throughout the year. The Tropics of Cancer and Capricorn, which mark the limits of the Sun's movement in this model, are seen as the boundaries of the tropics.

❄️ Polar Regions:
In this model, the polar regions experience extreme variations in daylight and temperature. During the northern hemisphere's summer, the North Pole is briefly exposed to the Sun for an extended period, resulting in the polar day. Conversely, during the northern hemisphere's winter, the North Pole is in darkness for an extended time, creating the polar night.

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