How did they form? 2025

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  1. Click ‘Get Form’ to open it in the editor.
  2. Begin by examining the objectives section. This will guide you on what students are expected to learn from the activities.
  3. Move to the background information about chondrites. Use this section to understand the context and significance of the meteorites being studied.
  4. Fill out the materials needed for each activity as listed. Ensure you have all items ready for a smooth execution of experiments.
  5. Follow the classroom procedure step-by-step, documenting observations and responses in the provided spaces. This is crucial for reflecting on learning outcomes.
  6. Finally, review your entries for clarity and completeness before saving or sharing your filled form.

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The super-hot core heated the mantle, which made the mantle lighter and caused it to rise up. This mantle was cooled at the ocean floor and became plates, or bedrock. These plates moved with the flow of the mantle and collided with other plates. At the boundaries where plates collided, lots of islands were formed.
The Earth formed over 4.6 billion years ago out of a mixture of dust and gas around the young sun. It grew larger thanks to countless collisions between dust particles, asteroids, and other growing planets, including one last giant impact that threw enough rock, gas, and dust into space to form the moon.
Earth formed around 4.54 billion years ago, approximately one-third the age of the universe, by accretion from the solar nebula. Volcanic outgassing probably created the primordial atmosphere and then the ocean, but the early atmosphere contained almost no oxygen.
Scientific evidence shows that the physical and behavioral traits shared by all people originated from apelike ancestors and evolved over a period of approximately six million years. One of the earliest defining human traits, bipedalism -- the ability to walk on two legs -- evolved over 4 million years ago.
The Earth formed more than 4 billion years ago along with the other planets in our solar system. The early Earth had no ozone layer and was probably very hot. The early Earth also had no free oxygen. Without an oxygen atmosphere very few things could live on the early Earth.

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The same goes for deep-sea hydrothermal vents. These chimney-like vents form where seawater comes into contact with magma on the ocean floor, resulting in streams of superheated plumes. The microorganisms that live near such plumes have led some scientists to suggest them as the birthplaces of Earths first life forms.
The giant-impact theory is most widely accepted today. This proposes that the Moon formed during a collision between the Earth and another small planet, about the size of the planet Mars. The debris from this impact collected in an orbit around Earth to form the Moon.

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