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===Magnetosheath=== {{main|Magnetosheath}} The magnetosheath is the region of the magnetosphere between the bow shock and the magnetopause. It is formed mainly from shocked solar wind, though it contains a small amount of plasma from the magnetosphere.<ref name=cluster>{{Cite book|editor1-last=Paschmann|editor1-first=G.|editor2-last=Schwartz|editor2-first=S.J.|editor3-last=Escoubet|editor3-first=C.P.|editor4-last=Haaland|editor4-first=S.|title=Outer Magnetospheric Boundaries: Cluster Results|journal=Space Science Reviews|date=2005|volume=118|issue=1β4|isbn=978-1-4020-3488-6|doi=10.1007/1-4020-4582-4 |url=https://cds.cern.ch/record/1250411/files/978-1-4020-4582-0_BookTOC.pdf|series=Space Sciences Series of ISSI|bibcode=2005ombc.book.....P }}</ref> It is an area exhibiting high particle [[energy flux]], where the direction and magnitude of the magnetic field varies erratically. This is caused by the collection of solar wind gas that has effectively undergone [[thermalization]]. It acts as a cushion that transmits the pressure from the flow of the solar wind and the barrier of the magnetic field from the object.<ref name="Van Allen"/>
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