Mercury has an average density of about 5.4 g/cm and a magnetic field. Normal rock has a density of about 3 g/cm. The magnetic field and higher density can be explained by O the melting of Mercury's rock by the Sun's heat, allowing it to be compressed by gravity O a larger than typical crust for a terrestrial planet O a substantial amount of iron (density around 8 g/cm) in a partially molten core

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Multiple C
Mercury has an average density of about 5.4 g/cm and a magnetic field. Normal rock has a derisity of about 3 g/cmº The magnetic field and higher density can
be explained by
O the melting of Mercury's rock by the Sun's heat, allowing it to be compressed by gravity
O a larger than typical crust for a terrestrial planet
O a substantial amount of iron (density around 8 g/cm) in a partially molten core
O Need help? Review these concept resources.
E Read About the Concept
Rate your confidence to submit your answer.
High
Medium
Low
Reading
O2022 McGraw Hill. All Rights Reserved.
Privacy Terms of Use
Transcribed Image Text:Multiple C Mercury has an average density of about 5.4 g/cm and a magnetic field. Normal rock has a derisity of about 3 g/cmº The magnetic field and higher density can be explained by O the melting of Mercury's rock by the Sun's heat, allowing it to be compressed by gravity O a larger than typical crust for a terrestrial planet O a substantial amount of iron (density around 8 g/cm) in a partially molten core O Need help? Review these concept resources. E Read About the Concept Rate your confidence to submit your answer. High Medium Low Reading O2022 McGraw Hill. All Rights Reserved. Privacy Terms of Use
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