CO and CO are discrete molecules, whereas the other oxides gain stability from extended bonding or ionic lattices. carbon's compact 2p orbitals overlap effectively with oxygen 2p orbitals, allowing strong multiple bonds that satisfy the valence requirements within small molecules. Intermolecular forces between CO or CO molecules are much weaker than those internal bonds, so low condensation temperatures and gaseous states at room conditions are unsurprising. CO is nonpolar overall but still has London dispersion forces and interactions between electric quadrupoles; “nonpolar” does not mean no attraction.
For larger Group 14 atoms, overlap with oxygen 2p orbitals is less effective for strong localized multiple bonding. SiO instead forms an extended network of SiO tetrahedra with each oxygen bridging two silicon atoms. Breaking or melting the network involves much more than separating intact SiO molecules. The Si–O electronegativity difference is , so these are strongly polar covalent bonds rather than evidence for a molecular solid.
For Pb–O the difference is , and ionic Pb/O or Pb/O descriptions provide useful starting points, with appreciable covalent contributions. PbO has layered structures with asymmetric oxygen coordination consistent with a stereochemically active 6s pair. A common PbO structure is rutile-like, with PbO octahedra linked through oxygen. Extended lattice interactions account for their solid states.[ref] The similar Si–O and Pb–O electronegativity differences show why a single difference threshold cannot determine the entire bonding type, coordination number or structure.

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