Lectures 10-11 • Autumn 2026

3D Crystallography &
Bravais Lattices

Named after Auguste Bravais (1848), discover how systematically extruding the 17 unique 2D plane groups into the third dimension enforces strict geometric constraints, yielding exactly 14 unique 3D lattice types.

Interactive Extrusion Engine

Deriving the 14 Bravais Lattices

Select any of the 17 plane groups below. Watch how symmetry elements (like mirrors and rotation axes) form infinite 3D boundaries. To prevent breaking these symmetries, the extrusion vector ($c$) must snap to specific alignments, revealing the 14 Bravais Lattices.

The 17 Plane Groups

Select to extrude

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Basal Plane (y=0)
Extruded Planes
Vector Paths
Extrusion Vector (c)
2D Unit Cell
3D Unit Cell
Mirror Plane
Glide Plane
2-Fold Axis
3-Fold Axis
4-Fold Axis
6-Fold Axis
Rigorous Analysis

Comprehensive Mapping of All 17 Plane Groups

Detailed breakdown mapping every single 2D plane group to its permitted 3D extrusion conditions, resulting crystal systems, and specific Bravais lattices.

Plane Group 2D Lattice Family Primary Symmetry Elements Extrusion Vector Condition ($c$) Resulting 3D System & Bravais Lattice
p1 Oblique None ($1$) Arbitrary direction ($c_x, c_y, c_z$) Triclinic (P)
p2 Oblique 2-fold axes ($C_2$) Orthogonal or Centered alignment Monoclinic (P or C)
pm Rectangular Mirror planes ($m$) Parallel shift or tilt along mirror plane Monoclinic (P, C)
pg Rectangular Glide planes ($g$) Parallel tilt (P), or half-cell offset along glide (C) Monoclinic (P or C)
cm Rectangular (Centered) Centered base + mirrors Parallel tilt along mirror plane Base-Centered Monoclinic (C)
pmm Rectangular Two orthogonal mirrors ($2mm$) Orthogonal (P), single-axis offset (C), or both-axis offset (I) Orthorhombic (P, C, or I)
pmg Rectangular Mirrors + Glides Orthogonal (P), single-axis offset (C), or both-axis offset (I) Orthorhombic (P, C, or I)
pgg Rectangular Orthogonal glides Orthogonal (P), single-axis offset (C), or both-axis offset (I) Orthorhombic (P, C, or I)
cmm Rectangular (Centered) Centered base + orthogonal mirrors Orthogonal or edge-centered shift Orthorhombic (C or F)
p4 Square 4-fold rotation ($C_4$) Orthogonal ($c \neq a$, $c = a$) or body/face-centered Tetragonal (P, I) & Cubic (P, I, F)
p4m Square 4-fold axes + mirrors ($4mm$) Strictly orthogonal or centered stacking Tetragonal (P, I) & Cubic (P, I, F)
p4g Square 4-fold axes + glides Strictly orthogonal or centered stacking Tetragonal (P, I) & Cubic (P, I, F)
p3 Trigonal / Hexagonal 3-fold rotation ($C_3$) Orthogonal stack or diagonal interlocking shift Hexagonal (P) & Trigonal/Rhombohedral (R)
p3m1 Trigonal / Hexagonal 3-fold axes + mirrors Orthogonal stack or diagonal shift Hexagonal (P) & Trigonal/Rhombohedral (R)
p31m Trigonal / Hexagonal 3-fold axes + alternate mirrors Strictly orthogonal stack Primitive Hexagonal (P)
p6 Hexagonal 6-fold rotation ($C_6$) Strictly orthogonal stacking Primitive Hexagonal (P)
p6m Hexagonal 6-fold axes + mirrors ($6mm$) Strictly orthogonal stacking Primitive Hexagonal (P)

Why can't pm, pg, or cm form an Orthorhombic Lattice?

In 3D, the defining symmetry of the Orthorhombic system is point group $222$, $mm2$, or $mmm$. This requires intersecting symmetry elements (like two orthogonal mirrors, or a mirror and a perpendicular 2-fold axis).

Plane groups like pm, pg, and cm contain only a single direction of symmetry planes (parallel mirrors or parallel glides). The only constraint these single planes impose on the extrusion vector ($c$) is that it must lie parallel to the plane. Because $c$ is free to tilt within that plane, it does not force an orthogonal $90^\circ$ angle. Therefore, the general symmetry it enforces is strictly Monoclinic.

While you could manually pull the vector perfectly straight up ($\alpha=\beta=\gamma=90^\circ$), this is merely an "accidental metric symmetry" (a pseudo-orthorhombic monoclinic cell). It does not upgrade the actual internal crystal symmetry to Orthorhombic because it still lacks that crucial second intersecting symmetry plane. To truly force an Orthorhombic Bravais lattice, you must start with a 2D plane group that already has orthogonal constraints, such as pmm, pmg, pgg, or cmm.

Systematic Overview

Summary of 3D Crystallography

Crystal System Unit Cell Properties Basic Symmetry Underlying Plane Group Point Groups (Schoenflies) Point Groups (Hermann-Mauguin) Space Groups
Triclinic (P) $a \neq b \neq c$
$\alpha \neq \beta \neq \gamma$
No symmetry p1 $C_1, C_i$ $1, \bar{1}$ 2
Monoclinic
(P, A/B/C or I)
$a \neq b \neq c$
$\alpha = \beta = 90^\circ, \gamma \neq 90^\circ$
2 or m p2, pm, pg, cm $C_2, C_s, C_{2h}$ $2, m, 2/m$ 13
Orthorhombic
(P, A/B/C, I, F)
$a \neq b \neq c$
$\alpha = \beta = \gamma = 90^\circ$
2mm pmm, pgg, pmg, cmm $C_{2v}, D_2, D_{2h}$ $mm2, 222, mmm$ 59
Tetragonal
(P, I)
$a = b \neq c$
$\alpha = \beta = \gamma = 90^\circ$
4 or 4mm p4, p4m, p4g $C_4, S_4, C_{4h}, C_{4v}, D_{2d}, D_4, D_{4h}$ $4, \bar{4}, 4/m, 4mm, \bar{4}2m, 422, 4/mmm$ 68
Rhombohedral (R) $a = b = c$
$\alpha = \beta = \gamma \neq 90^\circ$
3 p3, p3m1 $C_3, S_6, D_3, C_{3v}, D_{3d}$ $3, \bar{3}, 32, 3m, \bar{3}m$ 25
Hexagonal (P) $a = b \neq c$
$\alpha = \beta = 90^\circ, \gamma = 120^\circ$
6 and 3 p3, p3m1, p31m, p6, p6m $C_6, C_{3h}, C_{6v}, C_{6h}, D_6, D_{3h}, D_{6h}$ $6, \bar{6}, 6mm, 6/m, 622, \bar{6}m2, 6/mmm$ 27
Cubic
(P, I, F)
$a = b = c$
$\alpha = \beta = \gamma = 90^\circ$
4 and 3 or 2 and 3 p4, p4m, p4g $O_h, O, T_d, T_h, T$ $m\bar{3}m, 432, \bar{4}3m, m\bar{3}, 23$ 36
* The 32 Crystallographic Point Groups illustrate group-subgroup relationships indicating a descent in symmetry. Total Space Groups: 230.
Practice Assessment

Did It Sink In? - 10-11

Test your mastery of 3D lattice derivation, plane group extrusion constraints, and historical crystallographic trivia.

Take the Quiz