Showing posts with label non-Euclidean geometry. Show all posts
Showing posts with label non-Euclidean geometry. Show all posts

Thursday, May 18, 2017

Math Revisited: Non-Euclidean Geometry

My first exposure to non-Euclidean Geometry occurred in late 1963, as I put the finishing touches on my science fair project's  model of a “dual” universe, consisting of matter and antimatter in dynamic equilibrium. I proposed the hypothesis that matter and anti-matter universes co-existed not only in a kind of energy equilibrium, but one of coupled space as well. Thus, each mass-energy component occupied a differently curved space-time, both being non-Euclidean. One of these (matter) had positive curvature and the space-time was Riemannian (after Bernhard Riemann), while the other (anti-matter) had negative curvature and the space time was Lobachevskian (after Janos Bolyai and Nicholai Lobachevsky – who developed it).

In my actual model I employed a transparent sphere for a postively curved - Riemannian geometry and inside it, enfolded within, a negatively –curved opaque space. Thus did I portray both antimatter and matter in one superspace or super-manifold. For convenience – the two spaces are depicted separately above (Fig. 1), the positive (Riemannian) on the left, and the negative (Lobachevskian) on the right.

As can be ascertained by inspection (looking carefully at the meridian circles and latitude parallels in the Riemannian sphere), there are no two parallel lines in the Euclidean sense, since any two geodesics (curves of shortest path) must intersect(see Fig. 2 below)

. Thus, the sum of the angles of the triangle formed by 3 geodesics will always total > 180 degrees. Looking at the spherical geometry, it’s also easy to see why positively curved Riemannian geometry was the first to be developed – because it was based on the already familiar geometry of the sphere. (From which we use spherical trigonometry to obtain distances and angles, e.g. using a law of sines of the form: sin a/ sin(A) = sin b/ sin (B) where common letters refer to sides and capital letters to angles.)

Conversely, the angles on a negatively curved surface formed by three geodesics, always total less than 180 degrees. Also, on a negatively curved surface both the circumference and area of a circle increase faster (with increasing diameter) than for Euclidean space (the converse holds for the positively curved space).

Of course, at the time I didn’t realize the proper terms for the respective spaces were: elliptic (for Riemannian or +-curved), and hyperbolic (for Lobachevskian or negatively curved space. Nor did I appreciate at the time  that all three geometries – Euclidean, elliptic and hyperbolic were actually related to each other via a model known as the Poincare disk (Fig. 3).


In his disk model, Poincare depicted a hyperbolic plane within a Euclidean plane. The difference is that straight lines in Poincare’s disk once they are the same as geodesics (great circles) are warped. Thus, all straight lines on the disk appear to be curved lines – as shown – unless a particular line traverses the midpoint of the disk, in which case the apparent bending or warp is reduced to zero. So it appears as a straight line.

Another unique difference of the Poincare disk model from an ordinary circle is that the boundary of his model is infinitely far away or we would say “at infinity”. Another peculiar aspect concerns how right angles are formed and where. For example, the geodesic shown in the Poincare disk model makes right angles at either boundary. Similarly, any two geodesics that intersect (imagine another straight line 90 degrees different in orientation from that shown also passing through the disk center) form EUCLIDEAN angles at the point of their intersection.

Thus, the disk model is extremely valuable in that it permits discussion of non-Euclidean geometry in Euclidean terms. Let’s carry this forward looking at the curve PQ on the disk, and also the intermediary points A, B along it. Let’s assume we’d like to find the length x = AB, a segment of the curve PQ. Then one can show:

x = ln [(AQ/AP)/ (BQ/ BP)]

which uses a property common to natural logarithms called the ‘cross ratio’

Note the above definition contains embedded within the definition for points (A,B) , line (AB= x), length x, as well as “angle” – defined in terms of the Euclidean angle subtended at the point of intersection by tangents to the lines viewed as circular arcs in the putative Euclidean plane.

Let’s carry this forward looking at the curve PQ on the disk, and also the intermediary points A, B along it. Let’s assume we’d like to find the length x = AB, a segment of the curve PQ. Then one can show:

x = ln [(AQ/AP)/ (BQ/ BP)]

which uses a property common to natural logarithms called the ‘cross ratio’.  The above definition contains within it the definition for points (A,B) , line (AB= x), length x, as well as “angle” – defined in terms of the Euclidean angle subtended at the point of intersection by tangents to the lines viewed as circular arcs in the putative Euclidean plane.


. In the case of hyperbolic geometry the law of sines  takes a different one from that for spherical geometry (understandable given that the sum of angles in a hyperbolic triangle < 180 degrees!).  First, let’s recall the law of sines for the Euclidean case: 
a/ b = sin(A)/ sin(B).


For the spherical case:

Sin A/ sin a = sin B/ sin b = sin C/ sin c


where A, B, C denote ANGLES and a,b,c denote measured arcs.


Now for the hyperbolic case we have:
sin (A)/ sin(B) = {(sinh(a/k)/ sinh(b/k)}

where A, B, a, b again have the standard definitions as per angles and sides, and k denotes a positive constant that is often confused with curvature.  To be more specific, the value of k depends on the choice of the units of measurement. The value of k also expresses a definite length, all other factors being equal.

 For example, consider a number of concentric horocycles (such as QABP in Fig. 3) at a distance x from each other. Let their corresponding arcs have lengths: a1, a2, a3…..an. The ratio of each one to the next is then exp (x/k) where a1, a2, a3 etc. form a geometrical progression with the quotient:

exp (- x/ k) = 1  / (exp(x/k))

In other words, if the first arc is 1, the 2nd is 0.9, then the third is (0.9)2 = 0.81 and the fourth is (0.9)3  =  0.729 and so on.

 For those who may not know, “sinh” defines the hyperbolic sine. From calculus texts this is defined based on the exponential function, exp(x) as:

sinh(x) = ½ (exp(x) – exp(-x))

 with coordinates taken on the “unit hyperbola”: x2 – y2 = 1

 Similarly, the hyperbolic cosine (cosh(x)) is defined:


 cosh(x) = ½ (exp(x) + exp(-x))

In fact, when formulations are made one can obtain identities which parallel those of the standard trig functions. For example, in the latter we have:  cos2(x) + sin2(x) = 1, and in the hyperbolic sense one can prove:
 cosh2(x) - sinh2(x) = 1



 The hyperbolic cosine is useful to know when venturing into hyperbolic geometry because it is used to express a relation associating the 3 sides of a right triangle in hyperbolic space:
cosh(c/k) = cosh (a/k) cosh(b/k)

Many more detailed investigations of non-Euclidean geometry are possible, and also seeing how they link up with Euclidean geometry in a more general formalism. The basis for doing this entails taking a more comprehensive analytic (e.g. 'manifold') approach,  wherein we associate lines and points with a geometry. A simplified form for this may be expressed using the matrix formulation in 4(a). 


Where the left side denotes a line [u1, u2, u3]. If one finds that the point specified by (x1, x2, x3)  is the same as for another point specified (y1,y2, y3) such that the matrix relation in 4(b) is true then we can say that the correlation constitutes a polarity. It is possible that a suitable choice of polarity can be found for any combination of points for a line [u1, u2, u3] such that: u1 = x1, u2 = x2 and u3 = cx3.  In this case, if c = +1, the geometry is elliptic (e.g. Riemannian), and if c =-1 it is hyperbolic.   This gets us into the area of projective geometry.


Practice  Problems:

1. Consider a triangle in hyperbolic space as computed by an interstellar ship traversing it. The dimensions are: a = 1 pc, b = 2 pc and c is unknown where pc denotes parsec (1 pc = 3.26 light years).  Using this and the equation associating the 3 sides of a right triangle in hyperbolic space, with k = 1, find the dimension of c. Thence, find the ratios of the sines of the angles, e.g. (sin A/ sin B)

2. Consider the Lobachevskian surface shown in Fig. 1.  Assume  it displays concentric horocycles such that exp (- x/ k) =      1 / (exp(x/k)) and when the ratios for x/k are taken the progression is of the form: 1, 0.5, 0.25, 0.125 etc.  Use this to deduce the curvature k, if k = -1/ k2.  Is the non-Euclidean surface shown above a Riemannian or Lobachevskian space? Give reasons.




Saturday, April 12, 2014

How Much Advanced Math Preparation Do Middle and High School Teachers Need?



In a recent paper appearing in The Monthly Notices of the American Mathematical Society (Vol. 61, no. 3, p. 292-95) the question was asked as to how well Mathematics Teacher Education Programs Were “Aligned with Recommendations Made in MET II”?


Here “MET II” refers to the specific document:  The Mathematical Education of Teachers II. The thrust of the article then was to examine the extent to which the current preparation of Middle School math teachers (as well as High School math teachers) not only conformed with MET II recommendations but also the degree of integration between mathematics and pedagogy – and who should have a voice in making decisions about the preparation of mathematics teachers.

The article correctly notes:

“Little research has been done that examines the requirements of mathematics teacher education programs or the effects of these requirements.”

 
To try to answer the questions, the authors reported the “results of a national survey of secondary mathematics teacher education programs."  The main issue addressed was:

 
How much do current secondary mathematics teacher education program course requirements align with the recommendations described in MET II?”

 
In terms of the recommendations, they were categorized under those for: 1) prospective Middle School teachers and 2) prospective High School teachers,  as follows:

 
1)     Should be required to complete at least twenty four semester hours of mathematics that include at least fifteen semester hours on fundamental ideas of school mathematics appropriate for middle grades teachers.

2)     Should be required to complete the equivalent of an undergraduate major in mathematics that includes three courses with a primary focus on high school mathematics from an advanced viewpoint.

Whether given teaching programs conformed with the preceding or not was based on how respondents selected courses from a given list – for (1) and (2) respectively. The respondents were also to identify the total number of courses and credits for each course type. The final analysis of the paper used the data from 64 programs in respect of category (1) and 78 programs in respect of category (2).

The results obtained were interesting to say the least, including the following:

1) For Middle School Teaching Programs:

i) None of the programs reported using the MET II recommended fifteen semester hours of courses in fundamental ideas of school mathematics designed for middle grades teachers.

ii) The maximum number of required credits reported by any program was twelve semester hours (in four programs) and the average number of required credits of this type was three.

iii) The most commonly required programs were 'Geometry for Teachers' (13 programs), 'Statistics and Probability for Teachers' (4 programs) and 'Algebra for Teachers' (3 programs).

iv) 'Numbers and Operations' courses recommended by MET II were almost completely absent.

v) All 64 programs met the requirement for 9 semester hours of additional, advanced mathematics courses. Most university programs required teachers to take courses selected from statistics, calculus, number theory and discrete mathematics.  

vi) Calculus dominated, required in 63 of 64 programs, with Probability and Statistics next at 58 programs, and discrete mathematics with 45 programs requiring such courses.

 Aside:

For those unfamiliar with discrete mathematics, the following illustrate sample problems:

1. (a) Show that (p ® q)  «  (~q ® ~p)  is a tautology.                                       
    (b) Let x  Î { 2, 3, 4} and y Î {12, 16}.  Let the propositional function

P(x, y) be the statement “x is a factor of y”.  Write the following  propositions using conjunctions and disjunctions and determine the truth value of each.

            (i) "x $y P(x, y)              (ii) $y "x P(x, y)                                          


2.    (a)   Show that log n! = O (n log n).                                                                


(b)     Let f(x) = 2x3 + 3x –1 and g(x) =  log x. 

Find the least integer n such that:
 (fg)(x)=         
O(xn)                                                                                          
 
(c)Use mathematical induction to prove that

       (1x2) + (2x3) + (3x4) + … + n(n + 1)  =  n(n +1)(n +2)/3.                     

3.  (a) Prove that if n is an integer  and n3 + 5 is odd, then n is even using:
                        (i) indirect proof         (ii) proof by contradiction.   


Moving on,  let's look at the requirements:

2) For High School Teaching Programs:


i) Of the 78 programs that prepare high school teachers, sixty three or 81 percent, required a three course calculus sequence and the mean number of calculus courses across the programs was 2.8.

ii) Sixty nine programs (or 88 percent) required at least probability and statistics course.

iii) Almost all programs (76) required students to take at least one linear algebra course.

iv) MET II required 18 additional semester hours of advanced math beyond calculus, statistics and linear algebra courses and all the programs satisfied this requirement.

v) The most popular 'more advanced' math program was Geometry (70 programs), with Abstract Algebra next (61 programs) and then Discrete Mathematics (52).

vi) Only eight programs (10 percent) reported meeting the nine semester hours of high school mathematics from an advanced perspective. A typical description of such a course is shown below:

http://www.units.miamioh.edu/reg/bulletins/GeneralBulletin2012-2013/mth-409509-secondary-mathematics-from-an-advanced-perspective-3.htm


Some Observations:

In terms of the Middle School teacher preparation what amazed me the most is how few 'History of Mathematics' course programs were required. Make no mistake that the history of math gives the broad perspective I believe is needed for teaching at the middle grades (5-8) level. It also exposes the connections between the different math disciplines, i.e. between calculus and analytic geometry.  It would seem to me that Middle School teaching programs would be better served by more history of mathematics courses, than say Discrete Math.

Calculus dominates as it should, but anyone who's ever taught it also knows that the content can vary widely. What textbooks are being used, for example, and how useful are they to those being prepared? How much in the way of application is present?

In the Advanced Courses recommended for High School teaching programs I was somewhat dismayed to see the short shrift given to real analysis and differential equations (29% and 35% of programs adopted, respectively), say compared to geometry which appeared to dominate (90% of programs). WHY does geometry dominate? Looking back at secondary teaching programs from a historical perspective it appears it always has - going back to the 1920s (I have a relative's Geometry text from way back then, designated for teacher ed.)  All the same stuff you might expect is covered, including the theorems of Pappus and Desargues. But, if you're really going to teach Geometry why not use the best textbook of all, David Hilbert's Foundations of Geometry?

I suspect the predominance of Geometry, say in preference to real analysis and differential equations is because: 1) Most high schools still include at least one year of geometry in the curricula, despite the fact in the Caribbean and Singapore, for example, this is regarded as passé, and 2) Teachers- to- be are more comfortable with a course high in visualization content, as opposed to the more abstract real analysis, for example.

Inclusion of geometry at the secondary level is often expected in the same way as Algebra II - as a means to "encourage logical or critical thinking" - by having to manipulate objects in 2 or more dimensions. But I say if one is going to go this route it's far better to just replace it with solid geometry which can be more easily integrated with calculus (especially for AP students) or at least analytic geometry.  I warrant it's more important for a kid to know the equation for the ellipse (or the circle) and how to change them to change the shape and dimensions -i.e.  in terms of semi-major and semi- minor axis,  than to know Desargues theorem.

But old habits die hard, and it's probably going to take a long time before geometry is finally ousted from its preferential pedagogical perch.

As for teachers' exposure to geometry, they'd be better off just going through Euclid's Elements at a detailed level (say analogous to that presented in Stephen Hawking's book, God Created the Integers, Book I: Basic Geometry. Then follow it up by basic exposure to Non-Euclidean Geometry, say as provided in the excellent monograph: Non-Euclidean Geometry by Stefan Kulczycki.  Less time would be consumed and so more time could be devoted to really looking at the underlying math from an advanced perspective. In this sense, if one is later going to be faced with teaching algebra and geometry this would appear to be the better route to take, along with Abstract Algebra and at least 3 semester hours of History of Mathematics.


Sunday, March 23, 2014

Looking at Non-Euclidean Geometry and the Poincare Disk


















Thanks to Bernhard Riemann and Nikolai Lobachevsky, a rich alternate geometry was developed beyond the limits of Euclidean geometry.  It included using generalizations of the respective  triangles for which the sum of angles could be greater than 180 degrees (the Riemannian case) or less than 180 degrees.  The basic comparison of the two geometries is depicted in Fig. 1.This non-Euclidean geometry allowed itself to be paired to the advanced math of tensor calculus. (Which then was applied by Einstein to formulate his theory of general relativity).

As can be ascertained by inspection - looking carefully at the meridian circles and latitude parallels in the Riemannian sphere in Fig.2,-   there are no two parallel lines in the Euclidean sense, since any two geodesics (curves of shortest path) must intersect. Thus, the sum of the angles of the triangle formed by 3 geodesics will always total > 180 degrees.  Looking at the spherical geometry, it’s also easy to see why positively curved Riemannian geometry was the first to be developed – because it was based on the already familiar geometry of the sphere. (From which we use spherical trigonometry to obtain distances and angles, e.g. using a law of sines of the form: sin a/ sin(A) = sin b/ sin (B) where common letters refer to sides and capital letters to angles.)




















The proper terms for the respective spaces were: elliptic (for Riemannian or +-curved), and hyperbolic (for Lobachevskian or (-)-curved.

Interestingly,  all three geometries – Euclidean, elliptic and hyperbolic are actually related to each other via a model known as the Poincare disk (Fig. 3).


What Poincare achieved in his disk model is depicting a hyperbolic plane within a Euclidean plane. The difference is that straight lines in Poincare’s disk once they are the same as geodesics (great circles) are warped. Thus, all straight lines on the disk appear to be curved lines – as shown – unless a particular line traverses the midpoint of the disk, in which case the apparent bending or warp is reduced to zero. So it appears as a straight line.


Another unique difference of the Poincare disk model from an ordinary circle (which some will be tempted to assume or see) is that the boundary of his model is infinitely far away or we would say “at infinity”.  Another peculiar aspects concern how right angles are made and where they are made. For example, the geodesic shown in the Poincare disk model makes right angles at either boundary. Similarly, any two geodesics that intersect (imagine another straight line 90 degrees different in orientation from that shown also passing through the disk center) form EUCLIDEAN angles at the point of their intersection.



















Thus, the disk model is extremely valuable in that it permits discussion of non-Euclidean geometry in Euclidean terms. Let’s carry this forward looking at the curve PQ on the disk, and also the intermediary points A, B along it. Let’s assume we’d like to find the length x = AB, a segment of the curve PQ. Then one can show:


x = ln [(AQ/AP)/ (BQ/ BP)]

which uses a property common to natural logarithms called the ‘cross ratio’.  Note the above definition contains embedded within the definition for points (A,B) , line (AB= x), length x, as well as “angle” – defined in terms of the Euclidean angle subtended at the point of intersection by tangents to the lines viewed as circular arcs in the putative Euclidean plane.
 
Earlier, I showed the form the law of sines takes for spherical (elliptic) geometry. In the case of hyperbolic geometry it takes a different one from that (understandable given that the sum of angles in a hyperbolic triangle < 180 degrees!).  First, let’s recall the law of sines for the Euclidean case: 
 
a/ b = sin(A)/ sin(B).
 
Now for the hyperbolic case we have:
 
sin (A)/ sin(B) = {(sinh(a/k)/ sinh(b/k)}

where A, B, a, b again have the standard definitions as per angles and sides, and k denotes a positive constant that is confused with curvature!)  To be more specific, the value of k depends on the choice of the units of measurement. The value of k also expresses a definite length, all other factors being equal.

 For example, consider a number of concentric horocycles (such as QABP in Fig. 3) at a distance x from each other. Let their corresponding arcs have lengths: a1, a2, a3…..an. The ratio of each one to the next is then exp (x/k) where a1, a2, a3 etc. form a geometrical progression with the quotient:

 
exp (- x/ k) = 1  / (exp(x/k))

In other words, if the first arc is 1, the 2nd is 0.9, then the third is (0.9)2 = 0.81 and the fourth is (0.9)3  =  0.729 and so on.

 For those who may not know, “sinh” defines the hyperbolic sine. From calculus texts this is defined based on the exponential function, exp(x) as:

 
sinh(x) = ½ (exp(x) – exp(-x))

 with coordinates taken on the “unit hyperbola”: x2 – y2 = 1

 Similarly, the hyperbolic cosine (cosh(x)) is defined:

 cosh(x) = ½ (exp(x) + exp(-x))
 
In fact, when formulations are made one can obtain identities which parallel those of the standard trig functions. For example, in the latter we have:  cos2(x) + sin2(x) = 1, and in the hyperbolic sense one can prove:
 
 cosh2(x) - sinh2(x) = 1

 
 The hyperbolic cosine is useful to know when venturing into hyperbolic geometry because it is used to express a relation associating the 3 sides of a right triangle in hyperbolic space:
 
cosh(c/k) = cosh (a/k) cosh(b/k)

Many more detailed investigations of non-Euclidean geometry are possible, and also seeing how they link up with Euclidean geometry in a more general formalism. The basis for doing this entails taking a more comprehensive analytic (e.g. 'manifold') approach,  wherein we associate lines and points with a geometry. A simplified form for this may be expressed using the matrix formulation in 4(a). 

Where the left side denotes a line [u1, u2, u3]. If one finds that the point specified by (x1, x2, x3)  is the same as for another point specified (y1,y2, y3) such that the matrix relation in 4(b) is true then we can say that the correlation constitutes a polarity. It is possible that a suitable choice of polarity can be found for any combination of points for a line [u1, u2, u3] such that: u1 = x1, u2 = x2 and u3 = cx3.  In this case, if c = +1, the geometry is elliptic (e.g. Riemannian), and if c =-1 it is hyperbolic.   This gets us into the area of projective geometry.


 
 
 
 

 





 






Problems for Math Mavens:


1. Consider a triangle in hyperbolic space as computed by an interstellar ship traversing it. The dimensions are: a = 1 pc, b = 2 pc and c is unknown where pc denotes parsec (1 pc = 3.26 light years).  Using this and the equation associating the 3 sides of a right triangle in hyperbolic space, with k = 1, find the dimension of c. Thence, find the ratios of the sines of the angles, e.g. (sin A/ sin B)

2. Consider the Lobachevskian surface shown in Fig. 1.  Assume  it displays concentric horocycles such that exp (- x/ k) =      1 / (exp(x/k)) and when the ratios for x/k are taken the progression is of the form: 1, 0.5, 0.25, 0.125 etc.  Use this to deduce the curvature k, if k = -1/ k2.  Is the non-Euclidean surface shown above a Riemannian or Lobachevskian space? Give reasons.

Sunday, November 13, 2011

Is Science Resistant to Novelty? Not Really!




























In his recent WSJ column 'Mind and Matter' ('Is That Scientific Heretic a Genius or a Loon?'), p.C2, Nov 12-13, Matt Ridley ponders whether "scientific heretics" have been "persecuted" too often for their "radical ideas". He cites a number of examples including Daniel Schechtman who won a Nobel for the discovery of "quasi-crystals" when he was told earlier (by Linus Pauling) there was no such thing, "only quasi-scientists". Then there was Australian Barry Marshall, who ran a gauntlet of sorts when he hypothesized that bacterial infections caused stomach ulcers.

Then there was Charles Darwin, who postulated evolution by natural selection, and Albert Einstein, who proposed that planets orbit suns not because of a direct pulling action at long range (as Newton had proposed) but because a much larger mass object creates a curvature in space-time about which the smaller mass is constrained to move.

Using all these cases, Ridley then suggests that "science seems strangely resistant to novelty". Well, not really! You see, what an outsider or non-scientist may regard as "strangely resistant to novelty" in fact is the demand for rigor in showing that a new hypothesis is justified in effectively replacing or trumping hundreds of years of established science. Because a replacement of paradigm or model is indeed traumatic, overthrowing the life's work of thousands of dedicated minds, it is not taken lightly.

The issue then is not so much resistance to novelty, as insisting that whatever the "novelty" is it first pass a series of basic tests for falsification and also show how its own predictions enhance our understanding of the aspect of nature under scrutiny.

For example, Darwin early made a number of serious missteps before he was able to forge a coherent and correct theory! The problem was that in some cases, Darwin didn’t logically make the necessary connections that his observations actually disclosed, at the time he made them during his Beagle sojourn to the Galapagos.

Indeed, Darwin was so initially imbued with the creationist perspective that he failed to collect one single species of giant tortoise present in the islands. Fortunately, the occurrence of other species - and their recording- ultimately held away with the assistance of a consummate taxonomic researcher: John Gould - an ornithological expert at the London Zoological Society.

Indeed, had Darwin's mind already been "radicalized" to natural selection, and how adaptations operate within its purview, he'd have easily seen that the variety of beaks displayed among the Galapagos finches was directly traceable to the sort of foods they ate, in the respective islands. In point of fact, four of the fourteen finch species fed on seeds (as finches generally do), and another two species consumed fruits, flesh and flowers of cacti. Seven other finch species were primarily insectivorous, while one fed exclusively on leaves. Thus, from his creationist disadvantage point, it wasn't surprising that Darwin was fooled to the extent of believing some of the birds weren't finches at all.

According to Frank J. Sulloway, in his essay, ‘Why Darwin Rejected Intelligent Design’:

Faced with an absence of critical information to resolve the finches issue, Darwin continued to give a nod to the prevailing creationist assumption that variation within immutable species can lead to new varieties or subspecies that are adapted to local environments

Sulloway goes on to note that:

Darwin returned to England, on October 2, 1836. Three months later, he deposited his Beagle collections of birds with John Gould, the ornithological expert at the London Zoological society.”

He goes on to emphasize it was none other than Gould who “immediately realized the extraordinary nature of Darwin’s Galapagos specimens and analyzed and described them first

In other words, in a real sense, it was Gould who was the original radical thinker here and whose input then radicalized Darwin's!

Based on Gould’s analysis, contained in a full report he published March 1837, Darwin was finally informed that 3 of his 4 mockingbird species were distinct - new to science - and different from all other known mockingbirds. It was at that juncture Darwin found himself confronted by the problem of the origin of species that escaped him while actually in the Galapagos, imbued with his creationist mentality.

It would be no exaggeration to say Darwin was initially stunned by Gould's results. Indeed, if Gould was correct about the mockingbirds it meant that the supposed "barrier" between species had been broken by these birds on a set of isolated islands. Thus, gradual evolution through geographic isolation was the only plausible explanation that fit with the observational record (clarified by Gould, an expert ornithologist)

Darwin was later compelled to write in his Journal of Researches:"Seeing this gradation and diversity of structure in one small, intimately related group of birds, one might really fancy that from an original paucity of birds in this archipelago, one species had been taken and modified for different ends."

My point here is that Charles Darwin, contrary to the mythology circulated by those like Ridley, didn't suddenly arise as some instant maverick - like Zeus from Mount Olympus- but he had to be led in that direction by others first, and then re-process his original data to clarify it for himself, that he in fact observed and doumented what he did!

Then there was Albert Einstein, another poor guy who was allegedly initially impeded by the lethargic starched shirts of academe, to hear Ridley tell it. But not so fast! Einstein couldn't even begin to make sense of his own notions until he was able to incorporate non-Euclidean geometry into the picture as well as apply a comprehensive form of advanced mathematics known as tensor analysis (see attached image of Einstein writing one form of a tensor equation, i.e. R_ik - ½Rg_ik= 0 which can be rewritten, R_ik= 0 for the vacuum state, also known as "Ricci flat"). It was only after Einstein expended vast energy in formulating his curvature-tensor equations that HE was able to understand what it was he had accomplished, and could then make it comprehensible to others - including the basis for empirical tests such as the angle of deflection of a star's light passing near the Sun.

Thereby, Newton's theory of gravitation was more superseded in the context of a host of new uses and tests, as opposed to being "overthrown" by a crazed radical. For example, Newton's theory couldn't account for the bending of starlight near gravitating masses, but Einstein's could. Hence, General Relativity was used in these instances.

Neither could Newton's theory account for the solar oblateness (i.e. difference between polar and equatorial diameters), but Einstein's could to within a very good degree (though the Brans-Dicke theory of gravitation is giving some stiff competition). Finally, Newton's theory could say nothing whatever about gravitational lenses and lensing - now being incorporated into more and more distant, cosmological investigation. Einstein's could account for such lensing on the basis of curvature of space-time near gravitating masses.

Again, we see that the alleged sudden appearance of a "heretic" is nonsense! There is no "sudden appearance" because by the time the final hypothesis or theory was presented, the alleged heretic already had to undergo much difficult inner work and mental testing to make it sensible to himself!

When that doesn't happen, then really absurd embarrassments ensue. For example, Pons and Fleischmann's claim of "cold fusion" some 15 years ago, which was merely the result of them not adequately taking into account systematic errors in their apparatus. No one else was ever able to replicate any actual evolution of heat or energy in a lab at room temperature, under those conditions. Again, this shows the importance of moving very slowly and methodically and testing every step of the way. As the CERN team which claimed superluminal neutrinos already is, and which I predict will uncover extraneous sources of error hitherto unconsidered.

Finally, Ridley brings up another alleged "Heretic" in the person of one Henrik Svensmark. According to Ridley:

"In 1997, he suggested that the Sun's magnetic field affects the Earth's climate by shielding the atmopshere against cosmic rays, which would otherwise create or thicken clouds and thereby cool the surface. So he reasoned, a large part of the natural fluctuations ni the climate over recent millennia might reflect variation in solar activity."

But I already skewered the basis for this nonsense in a previous blog:

http://brane-space.blogspot.com/2010/12/carbon-isotope-ratios-and-climate.html

Which also showed a critical graph (see attached) , bearing a 2000-year record of C14:C12 ratio deviations as been compiled by P.E. Damon ('The Solar Output and Its Variation', The University of Colorado Press, Boulder, 1977) . As solar physicist John Eddy has pointed out:

The gradual fall from left to right (increasing C14/C12 ratio) is…probably not a solar effect but the result of the known, slow decrease in the strength of the Earth’s magnetic moment.[1] exposing the Earth to ever-increased cosmic ray fluxes and increased radiocarbon production.

The sharp upward spike at the modern end of the curve, representing a marked drop in relative radiocarbon, is generally attributed to anthropogenic causes—the mark of increased population and the Industrial Age"

But evidently the Über-radical Svensmark was in such a heated hurry to establish his heresy he didn't bother to examine the work already done on the solar-cosmic ray- climate nexus by Eddy and Damon!

Ridley then continues his pseudo-heretic promotion:

"Dr. Svensmark is treated as a heretic mainly because his theory is thought to hinder the effort to convince people that recent climate variation is largely manmade, not natural, so there is his bias toward resisting the idea"

Actually, that's largely bollocks and the reason is that one part of his theory ( a slowing magnetic cycle or cooler Sun) has already been proven wrong as the Sun ramps up its activity once again. Meanwhile, Svensmark was one of those who erroneously construed the data in a Nature paper by Dr. Noel Keenlyside et al, i..e. that cooling has been occurring since 1997,. and that doesn't put his statistical acumen in much stead.

In addition, as I showed above, the much longer term studies of Damon and Eddy totally refute Svensmark's hypothesis of a cosmic ray-cloud based natural variant of climate change, in the sense of controverting the anthropogenic warming hypothesis, via CO2 - accepted now by more than 97% of the climate scientists of the planet (Eos Transactions of the American Geophysical Union, Vol. 90, No. 3, p. 22) .

Ridley then refers to the recent CERN (CLOUD) studies on cosmic rays and climate variation, and implies that those will finally bear out the great rebel Svensmark's theories. Even Svensmark appears to agree as he said in one recent online interview:

"I welcome the CLOUD results. They basically confirm our own experimental results since 2006, and does so within a larger variation of parameters. It seems to say that ions are fundamental for the nucleation of new aerosols."

But again, I shot this crap down in another blog:

http://brane-space.blogspot.com/2011/09/cosmic-ray-blarney-will-flat-earther.html

in which I noted, regarding one of the CLOUD team's results :

"Kirkby and his colleagues were nevertheless cautious on the finding as they also reported that the presence of certain atmospheric pollutants, such as H2So4 (which can incept "acid rain"- which appears when water molecules in the atmosphere react with sulphur dioxide or SO2). In that case, seed formation is repressed by up to 1/1000 of those needed to account for cloud seeding. Worse, it's already known that clouds are very poorly parameterized in climate models as a whole. This has led to an ongoing debate over the past 8 years on whether in fact the sign of albedo change is positive or negative. (See e.g. ‘Can Earth’s Albedo and Surface Temperature Increase Together’ in EOS, Vol. 87, No. 4, Jan. 24, 2006, p. 37).

Ridley wages a column bet that based on his work, Svensmark "may yet prove to be a Schechtman".

I'd say, based on what I've seen, it's more likely he'll prove to be a Pons or Fleischmann!