model specific heat as a function of temperature for a number of typical meteorite classes with known mineralogical compositions. We present, as examples, thecP(T) curves of a number of well-described laboratory regolith analogs, as well as for planetary ices and ‘tholins’ in the outer solar...
The Three Major Types of Rocks | Definition & Examples 6:32 Ch 7. Igneous Rocks Ch 8. Volcanic Landforms Ch 9. Weathering and Erosion Ch 10. Sedimentary Rocks: A Deeper Look Ch 11. Metamorphic Rocks: A Deeper Look Ch 12. Rock Deformation and Mountain... Ch 13. Water Balance on Ear...