As lanthanides are extracted in greater amounts and find further applications, knowledge of the speciation of their labile solution species becomes increasingly important. So far, most effort has been directed to understanding the aqua ions, and particularly the first coordination sphere, using information largely from diffraction studies on crystalline salts and lately upon solutions. For the lighter and larger early lanthanides, it is believed that nine‐coordinate trigonal prismatic [Ln(OH
2
)
9
]
3+
ions predominate for the early metals (Ln = La‐Nd), and that square antiprismatic eight‐coordinate [Ln(OH
2
)
8
]
3+
ions are characteristic of yttrium and the later lanthanides (Ln = Gd‐Lu); a mixture of eight‐ and nine‐coordinate species is associated with Ln = Pm‐Eu. For the slightly smaller scandium aqua ion, it is believed that [Sc(OH
2
)
n
]
3+
has a coordination number of 7 or 8. The coordination numbers are not always the same in crystalline salts as in solution; in particular, octahedral [Ln(OH
2
)
6
]
3+
ions have been found in crystalline perchlorate salts that are not found in solutions of the perchlorates. Addition of coordinating ions such as chloride leads to isolation of solid salts that contain ligands other than water in the coordination sphere, while nitrate coordinates to these metals as a bidentate ligand. Study of the ions in nonaqueous solvents in the presence of weakly coordinating anions has led to the identification of a number of simple solvated species, such as [Ln(dmso)
8
]
3+
, though again there is evidence for mixed coordination, such as seen with the eight‐ and nine‐coordinate [Ln(dmf)
n
]
3+
and [Ln(MeCN)
n
]
3+
(
n
= 8, 9).