Jump to content
Toggle sidebar
The Portal Wiki
Search
Create account
Personal tools
Create account
Log in
Pages for logged out editors
learn more
Talk
Contributions
Navigation
Intro to The Portal
Knowledgebase
Geometric Unity
Economic Gauge Theory
All Podcast Episodes
All Content by Eric
Ericisms
Learn Math & Physics
Graph, Wall, Tome
Community
The Portal Group
The Portal Discords
The Portal Subreddit
The Portal Clips
Community Projects
Wiki Help
Getting Started
Wiki Usage FAQ
Tools
What links here
Related changes
Special pages
Page information
More
Recent changes
File List
Random page
Editing
The Road to Reality Study Notes
(section)
Page
Discussion
English
Read
Edit
View history
More
Read
Edit
View history
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
===2.5 Other representations of hyperbolic geometry=== Since hyperbolic geometry is a more abstract construct, the ''conformal'' representation presented in section 2.4 is not the only way to represent hyperbolic geometry in terms of Euclidean geometry. ''Projective'' representations are next presented, where the difference is that hyperbolic straight lines are now represented as Euclidean straight lines. The cost of this ‘simplification’ is that angles are no longer the same. Penrose gives the reader an equation which allows the ''projective'' geometry to be obtained from a radial expansion from the center of the ''conformal'' representation. The geometer Eugenio Beltrami is introduced as having discovered a geometric method relating these different hyperbolic representations which involve projections from the plane to spherical surfaces and back. Imagine the hyperbolic plane cuts a sphere at the equator. ''Hemispheric'' representation is the hyperbolic geometry representation on the northern hemisphere of the Beltrami sphere, found from projecting the ''projective'' representation upward onto its surface. Straight Euclidean lines in the plane are now semicircles which meet the equator orthogonally. Stereographic projection is introduced with the example of projecting these semicircles back onto the plane but projecting from the point of the south pole. This beautifully gives us the ''conformal'' representation on the plane. Two important properties of stereographic projection are: * Conformal, so angles are preserved * Sends circles on the sphere to circles on the plane It is then emphasized that each of these representations are merely ‘Euclidean models’ of hyperbolic geometry and are not to be taken as what the geometry actually ‘is’. In fact, there are more representations such as the [https://en.wikipedia.org/wiki/Minkowski_space Minkowskian geometry] of special relativity. The idea of a generalized ‘square’ is then presented in ''conformal'' and ''projective'' hyperbolic representations to show an interesting generalization of the Euclidean square.
Summary:
Please note that all contributions to The Portal Wiki may be edited, altered, or removed by other contributors. If you do not want your writing to be edited mercilessly, then do not submit it here.
You are also promising us that you wrote this yourself, or copied it from a public domain or similar free resource (see
The Portal:Copyrights
for details).
Do not submit copyrighted work without permission!
Cancel
Editing help
(opens in new window)