Makemake
Makemake is a dwarf planet located in the Kuiper Belt, a region of the outer Solar System. It was discovered in 2005 by a team of astronomers led by Mike Brown.
Characteristics of Makemake
Makemake is known for its reddish-brown color and its relatively low density. It is the second brightest object in the Kuiper Belt after Pluto. Its surface is covered in frozen methane, ethane, and possibly nitrogen, giving it a distinct appearance.
Orbital and Physical Characteristics
Makemake has an orbital period of about 310 years and is located at an average distance of 45 astronomical units (AU) from the Sun. It has a diameter of approximately 1,430 kilometers, making it smaller than Pluto and Eris, but larger than Haumea.
Study Guide
- What is the location of Makemake in the Solar System?
- Who discovered Makemake and in what year?
- Describe the surface composition of Makemake.
- How does the orbital period of Makemake compare to that of Earth?
- What is the approximate diameter of Makemake?
◂Science Worksheets and Study Guides Sixth Grade. Earth's Atmosphere
Study Guide
Earth's Atmosphere 
Activity Lesson
Earth’s Atmosphere Worksheet/Answer key
Earth's Atmosphere Worksheet/Answer key
Earth's Atmosphere Worksheet/Answer key
Earth's Atmosphere Worksheet/Answer key
Earth's Atmosphere Vocabulary/Answer key
Earth's Atmosphere Vocabulary/Answer key
Earth's Atmosphere Vocabulary/Answer key
Earth's Atmosphere Vocabulary/Answer key
Earth's Atmosphere Vocabulary/Answer key
Earth's Atmosphere Vocabulary/Answer key
Earth's Atmosphere Vocabulary/Answer key
Earth's Atmosphere
Activity LessonWorksheet/Answer keyWorksheet/Answer keyWorksheet/Answer keyWorksheet/Answer keyVocabulary/Answer keyVocabulary/Answer keyVocabulary/Answer keyVocabulary/Answer keyVocabulary/Answer keyVocabulary/Answer keyVocabulary/Answer keyThe resources above cover the following skills:
EARTH AND SPACE SCIENCE
Earth’s Systems
Use models (e.g., diagrams, maps, globes, digital representations) to explain how the rotation of Earth and unequal heating of its surface create patterns of atmospheric and oceanic circulation that determine regional climates.