Geography Reference
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2 R . In contrast, Fig. 4.2 presents the helicoid and the one-sheeted
hyperboloid of revolution as alternative examples of a ruled surface.
the circular cone of the sphere S
2
R cos Φ 0
2
Example 4.1 (Circular cone
C
of the sphere
S
R ).
2
Let us construct a circular cone of the sphere
R as a ruled surface. First, we choose the parallel
circle, also called small circle , of the parameterized sphere as the reference curve or directrix.
Second, we attach locally to any point of the directrix a vector field which is generated by a
ruler moving along the reference curve. Consult Box 4.1 and Fig. 4.1 for a more detailed analysis.
In terms of spherical coordinates
S
, we parameterize the “position vector” X ( Λ, Φ, R )
with respect to an orthonormal frame of reference { E 1 , E 2 , E 3 |O} , spanning a three-dimensional
Euclidean space E
{
Λ, Φ, R
}
2 R of radius
R . {C Λ ,C Φ |Λ, Φ} is the local frame of reference i.e. Cartan's moving frame (“repere mobile”),
attached to a point {Λ, Φ}∈ S
3 , attached to the origin O , which is the center of the sphere S
2 R . As the reference curve, we have chosen the parallel circle Φ 0 =
constant, namely the directrix x ( U ), where U = Λ is the parameter of the reference curve. The
generator or the ruler of the surface is the vector field Y ( U ):= C Φ ( U ), the unit vector which is
normal to C Λ ( Λ, Φ 0 ), directed towards North. The linear manifold V Y ( U ), also called the bundle
of straight lines , is forming the circular cone
of radius R cos Φ 0 as soon as the ruler moves
around the parallel circle. Finally, we have gained the parameterized ruled surface X ( U, V ). Its
typical matrix of the metric, G, has been computed.
C
2 R cos Φ 0
End of Example.
Additionally, let us more precisely define a ruled surface in Definition 4.1 , which follows after
Box 4.1 summarizing the vector definitions of Example 4.1 .
2 R : ruled surface).
Spherical coordinates and Cartan's frame of reference:
2 R cos Φ 0
Box 4.1 (Circular cone
C
of the sphere
S
R cos Φ cos Λ
R cos Φ sin Λ
R sin Φ
,
X ( Λ, Φ )=[ E 1 , E 2 , E 3 ]
(4.1)
sin Λ
+cos Λ
0
D Λ X ( Λ, Φ )
,
C Λ :=
=[ E 1 , E 2 , E 3 ]
(4.2)
D Λ X ( Λ, Φ )
sin Φ cos Λ
sin Φ sin Λ
cos Φ
D Φ X ( Λ, Φ )
.
C Φ :=
=[ E 1 , E 2 , E 3 ]
D Φ X ( Λ, Φ )
Directrix x ( U ) (parallel circle, small circle, curve of constant latitude Φ 0 ,U = Λ ):
R cos Φ 0 cos U
R cos Φ 0 sin U
R sin Φ 0
.
x ( U ):=[ E 1 , E 2 , E 3 ]
(4.3)
Generator or ruler of the surface ( U = Λ ):
 
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