(with a ≠ 0) in some Cartesian coordinate system.
Solving for y leads to the explicit form
Solving the implicit equation for x yields a second explicit form
can also be deduced from the implicit equation by putting 
The semicubical parabolas have a cuspidal singularity; hence the name of cuspidal cubic.
Any semicubical parabola is similar to the semicubical unit parabola .
Proof: The similarity (uniform scaling) maps the semicubical parabola onto the curve with .
Differentiating the semicubical unit parabola one gets at point of the upper branch the equation of the tangent:
This tangent intersects the lower branch at exactly one further point with coordinates 
(Proving this statement one should use the fact, that the tangent meets the curve at twice.)
Determining the arclength of a curve one has to solve the integral For the semicubical parabola one gets
(The integral can be solved by the substitution .)
Example: For a = 1 (semicubical unit parabola) and b = 2, which means the length of the arc between the origin and point (4,8), one gets the arc length 9.073.
The evolute of the parabola is a semicubical parabola shifted by 1/2 along the x-axis:
In order to get the representation of the semicubical parabola in polar coordinates, one determines the intersection point of the line with the curve. For there is one point different from the origin: This point has distance from the origin. With and ( see List of identities) one gets 
Mapping the semicubical parabola by the projective map (involutoric perspectivity with axis and center ) yields hence the cubic function The cusp (origin) of the semicubical parabola is exchanged with the point at infinity of the y-axis.
This property can be derived, too, if one represents the semicubical parabola by homogeneous coordinates: In equation (A) the replacement (the line at infinity has equation .) and the multiplication by is performed. One gets the equation of the curve
Choosing line as line at infinity and introducing yields the (affine) curve
An additional defining property of the semicubical parabola is that it is an isochrone curve, meaning that a particle following its path while being pulled down by gravity travels equal vertical intervals in equal time periods. In this way it is related to the tautochrone curve, for which particles at different starting points always take equal time to reach the bottom, and the brachistochrone curve, the curve that minimizes the time it takes for a falling particle to travel from its start to its end.
The semicubical parabola was discovered in 1657 by William Neile who computed its arc length. Although the lengths of some other non-algebraic curves including the logarithmic spiral and cycloid had already been computed (that is, those curves had been rectified), the semicubical parabola was the first algebraic curve (excluding the line and circle) to be rectified.[disputed (for: It appears that parabola and other conic sections have been rectified a long time before) ]