C OMPOSITIO M ATHEMATICA
T HOMAS A. S CHMIDT
M ARK S HEINGORN
On the infinite volume Hecke surfaces
Compositio Mathematica, tome 95, n
o3 (1995), p. 247-262
<http://www.numdam.org/item?id=CM_1995__95_3_247_0>
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On the infinite volume Hecke surfaces
THOMAS A. SCHMIDT* & MARK
SHEINGORN~
©
*Oregon State University, Corvallis, OR 97331; tBaruch College, Cuny, New York, NY 10010
Received 28 September 1993; accepted in final form 6 January 1994
Abstract. An infinite volume Hecke surface, G03BBBH, is the Riemann surface associated with the Hecke triangle group of translation length 03BB > 2. This paper: (i) gives an algorithm producing the length spectrum for each of these surfaces employing an unramified double cover (by way of illustration, we tabulate the shortest 25 geodesics for the case À = 4. We know of no other infinite volume surface for which this data exists). (ii) Establishes the existence of a Hall ray for open
geodesics on G03BBBH. Our proof requires that >
J8.
The existence of a Hall ray means (after Haas) that the set consisting of the highest penetration of each geodesic into the fundamentalhorocycle is dense in some real half-line. It is necessary to use open geodesics-there is no Hall
ray otherwise. This is in marked contrast to the finite volume case, as we prove.
1. Introduction
The
length
spectrum of a Riemannsurface,
the sequence oflengths
of closedgeodesics,
has been theobject
of intensestudy
since at least the advent of theSelberg
TraceFormula,
which involves this spectrum in a crucialmanner. For more on these matters, we refer the reader to Peter Buser’s recent book
[Bu].
There has also been recent
activity
in thestudy
of thelength
spectrum(especially
asmoduli)
in moregeneral
differentialgeometric settings,
forexample
see Croke[C]
andLalley [L]. Chiefly,
this paper offers theexplicit computation
of thelength
spectrum of a one real parameterfamily
ofinfinite volume surfaces with ramification 2013the Hecke
triangle
surfaces of the second kind. Mostprevious explicit computation
has takenplace
on asingle
finite volumesurface, although
ourprevious
paper[S-S]
discussescomputations
for all finite volume Hecketriangle
groups. We know of noother infinite volume surface for which such
computations
exist in the literature.(However,
the referee haskindly pointed
out that there arealgorithms
and(unpublished) computations
for surfaces with apositive
lower bound for the
injectivity
radiustogether
with a free fundamental group. In this paper said lower bound is zero due to the cusp, and the surface isramified.) Fittingly perhaps,
it turns out that for theseexamples
the shortest
geodesic
is theboundary geodesic.
Our second set of results concerns the existence of a Hall ray
(defined below)
for various classes ofgeodesics.
In the case of the modular group, the existence of the Hall ray for closedgeodesics
iséquivalent
to theexistence of the Hall ray for the Markoff spectrum
(this
lastdepends
onHall’s theorem to the effect that every real number in
[0, 1]
may berepresented
as the sum of tworegular
continued fractions(CFs)
withpartial
denominators less than4;
thus the name Hallray).
This argument goes over, mutatismutandis,
to the finite volume Hecketriangle
groups. Notunexpectedly,
the role of the CFs isplayed by
the(Rosen-like [R])
next03BB-CFs
already
used in[S-S].
But,
as we prove, Hecke groups of the second kind do not have a Hall’s ray if we are restricted to the useof (the
very sparse setof)
closedgeodesics.
We must also
employ
opengeodesics indeed geodesics
with ends in the funnel(almost
allgeodesics
have thisproperty).
Here thetechnique
ofestablishing
the existence of the Hall ray isgeometric,
not continuedfraction based.
Haas-Series
[H-S]
referred to the sequence of closedgeodesic
penetra- tions as the Cohn spectrum. Asabove,
the Cohn spectrum and the Markoff spectrum coincide for finite volume Hecke groups. The remarks of theprevious paragraph
show that these notions bifurcate for infinite volume(second kind)
Hecke groups.We thank A. Haas for
pointing
out an error in theoriginal
version ofthis work and the referee for
help
inimproving
thepresentation.
2.
Geometry
andlength
spectrum ofH03BBBH
The Hecke group
G03BB is
the Fuchsian groupwhich,
when considered asacting
upon the Poincaré upperhalf-plane,
isgenerated by
S : z ~ z + 03BB andT:
z~ 2013 1/z.
When 03BB >2, GA
is of the secondkind;
thatis,
it is a group of infinite volume. We consider thesubgroup H.
of index 2 inG.
defined asfollows:
These generators are
obviously parabolic;
we denote themP1 and P2,
respect-ively.
Thesignature
ofH03BBBH
is(0;
oo,~;1); i.e.,
asphere
with twopunctures
and one hole.Pi
andP2 are conjugated
into one anotherby T,
which means that this is a non-trivial rotationalisometry
of the surface thatinterchanges
thecusps. This rotation fixes
(the projection of)
i andinterchanges
those ofFig. 1. Fundamental région for HA.
±2/Â
+i~1-4/03BB2,
which are"antipodal"
on theboundary geodesic.
Theselast are, of course, identical when
projected
toG03BBBH.
The virtues of
working
this surface are thatH03BB
isfreely generated by P1 and P2 thus, H03BB
is amanifold,
notmerely
an orbifold. This feature makes themanner in which short
geodesics
are constructedquite
"visual". A fundamentalregion
for this group isgiven just
below. It should be notedthat,
theboundary geodesic,
thehole,
and theprojection
of i(which
is anordinary point
onH03BBBH,
ofcourse)
aresymmetrically placed
with respect to the cusps.(More precisely
each isfixed,
butonly
ipoint-wise, by
T, which is anisometry
ofH03BBBH.)
We are
going
togive
bounds for the trace ofcyclically
reduced words inP
1and
P2.
This is doneby estimating
thelength
contributed to a closedgeodesic by: (i)
the presence of a termPi
in its word(|n|
>1). (The
contribution of a term inP2
will be the same since theconjugation by T,
anisometry, interchanges these.) (ii)
The presence of consecutive terms of the formP1 . P-t2;
s, t = ± 1. Note that a closed
geodesic
must remain inside the Nielsen convexregion
X forG.,
else it iscaptured by
the funnel and cannot be closed.Consider the array of fundamental
regions
forH03BB given by
the one aboveand all translates
by
S±m forintegral
m. The array has a sequence ofpairs
ofsides
terminating
at(anchored at) ±mÂ.
The presence of a termPn1
in a word isequivalent
to the presence of a segment of thecorresponding geodesic
connecting
two of the abovepairs
anchored atpoints
nl apart. Such a segment haslength
at mostd(1/03BB+i/03BB,n03BB-1/03BB+i/l)=2logn+4log03BB+O(1), by
Beardon
([Be], Eq. 7.2.1(i))
and also theheight
of theboundary geodesic (given below). Similarly,
it haslength
at leastd(i, n03BB + i)
=2 log
n +21og
 +0(l).
Note that the
sign
of nmerely
determines the direction in which the segment istraversed,
not itslength
and that this estimate works even when n = 1.We have shown:
LEMMA 1. The
length of the geodesic given by
acyclically
reducedhyperbolic
wordis less than
1 t is greater than E
03A3jlog(|aj| + |bj|).
For each runof
nconsecutive j
withlajl
=lbjl
=1, Fn log 03BB is
added to thelength. (Here B, C, D,
E and F areindependent of À.)
Of course this is
equivalent
to acorresponding
bound on the trace of A. Increating
ouralgorithm
for thelength
spectrum ofG.,
we needonly
resolve anyambiguities arising
from the above statementbeing
with respect to a doublecover of our basic groups. That
is,
we must locate those words(A c- H.,
listedout as
above)
which have square roots inG..
This iseasily
done via the sametechnique
weemployed
in[S-S] : i.e., obtaining
a CFexpansion
of a fixedpoint
of
A,
andchecking
for a shorterperiod.
Using
Lemma1,
one can create acomplete
list of shortestgeodesics
onH03BBBH.
Here is a way to visualize the process. Geodesics onH03BBH
may be described aswinding
about a cusp, thentraversing
at least half of theboundary geodesic (with
morewinding
about the hole apossibility),
and thenwinding
about the other cusp, and so on. Each of these processes adds an estimable amount of
length
to thegeodesic. (Cusp loops
withcorresponding
behavior atthe cusps are isometric via
T.)
Here is the dataprecisely:
Boundary geodesic:
This iseasily
shown to be fixedby
the(primitive
inHJ hyperbolic
the first power of the latter
being
inG03BB - H,,.
Thelength
isthus z 2 log À.
Therefore
winding
about the hole m times adds ~ 2mlog
03BB to thelength. (Here
m may be a
half-integer.)
Loops
about a cusp:Up
to a constantindependent
ofÀ, looping
about a cuspm times adds no more than
d(ilÀ,
m +ilÂ)
and no less thand(i,
mÀ +i). (The
former comes from the fact that the
boundary geodesic
runs betweenGeodesic
loops
must stay "above" thisgeodesic,
elsethey
arecaptured by
thefunnel.)
From this it is easy to compute the addedlength as ~ log m
+2 log Â.
As an
example, PT. Pl
isjust Pm-11·P1P-12·Pn+12.
This is n - 1trips
aboutoo, half the
boundary geodesic,
and m + 1trips
about zero. It is easy todirectly
compute the trace of
PT. P2,
and this has the same order ofmagnitude (with
respect to m andn)
as the estimates from Lemma 1.3. The
length
spectrum ofG).. B31’
With an obvious abuse of
notation,
let S and T be the usual matrixrepresentatives
of the above elements S and T. Let U =ST;
we definegi =
Ui-1 S and hi
=Tgi-1 T.
Infact, hi
is the transpose of gi. Letf/m
={gi, hi}mi=
1 and J =Um f/m.
We say that a word W in S and T is T-reduced if T appears in W to at most the first power.
LEMMA 2. Each
conjugacy
classof GI,
other than thoseof
Tand {Uj}~j=
1has a
representative
which is a word in ,91 withonly positive
exponents.Proof.
The finite covolume Hecke groups are of the formG03BBq(=: Gq, by
abuse of
notation),
withÂq
= 2 cos03C0/q and q ~
3 aninteger.
Therelations in
Gq
are T2 = Uq = I. Thesegive
rise to g[q/2]+j= hj for j
=1,
... ,[q/2]. With q
and Àfixed,
we have thehomomorphism
There is an
injective
set-map(but
not ahomomorphism)
which takes aT- and U-reduced W of
G qto
the same word in the generators ofG.,
The ~q
are notinjective,
but are stable in the sense that for any reduced W inGÂ,
there is aninteger Q(W)
such that forall q
>Q(W), W
=iq(~q(W)). Indeed, Q(W )
issimply
thelargest
exponent of U orU -1
to befound in
W;
themeaning
here is that~q(W)
is reduced inGq
with respectto
T2
= I and Uq =I. We note thatQ(iq(Aq))~q
for any reducedAq
ofGq .
Given reduced W of
G03BB, let q
>Q(W)
beodd,
then[S-S]
shows that theG -conjugacy
class of~q(W)
has a memberexpressible
inpositive
terms of{gq,i, hq,i}[q/2]i=1.
LetAq~q(W)A-1q
be such aconjugate.
Let A =iq(Aq).
Since9j =
iq(gq,j)
andsimilarly
forhj,
we are done.REMARK.
Although
the above could beproved
in a more direct manner,the stratification of
G03BB by q-stably
reduced sets, theiq(Gq),
is the avatar inthe structure of the infinite volume
G03BB
of what we called the"q principle"
in
[S-S].
We arestressing
that a T- and U-reduced word forGq
is also sucha word for
Gq,
for allq’
> q.Indeed,
for allG03BB
with >03BBq.
And since U"appears in a
given
T-reduced word W ofG03BB
to a maximal exponent, W may bethought
of asbeing
"in"Gq
forall q
>Q(W).
For theGq,
themanner in which the
geometric
aspects of theseimages
of Wdepend
on q isexactly
what we calledthe q principle.
We take theopportunity
here topoint
out that the fact that the theta group,Gq=~
is the limit of theGq
hasbeen
given
the name of "discrete deformation" and the fact that everyfinitely generated
Fuchsian group with cusps admits such alimiting
sequence of Fuchsian groups with a chosen cusp of the
original
groupbeing replaced by elliptics of increasing
order has been shownby
J. Wolfart[W].
The
importance
of J is that all of its elements may be taken as matrices withnon-negative
entries. Inparticular,
traces ofproducts (other
than thoseof the form
gm1
orhm1)
increase. The ideas of B. Fine[F]
can beapplied,
asin
[S-S],
to obtain trace-classrepresentatives
in order of size of trace andthereby
to list out all closedgeodesics
in order oflength.
The
only
closedgeodesic
which does not arise from an J-word is the closedgeodesic
fromIn
[S-S]
it was shown thattr(g q,j)
>tr(gq,j-1)
for all2 ~ j ~ [q/2].
Astr(hj)
=tr(gj),
the same is true for thehj.
Call the sum of the exponents in a reduced word W of J the block
length
of W ForG,,,
thehyperbolic
elements of blocklength
1give
theshortest
geodesics.
This is nolonger
the case forGÂ. Indeed,
theboundary
geodesic corresponding
to U is the shortestgeodesic
onG03BB. But,
there arealso
hyperbolics
ofhigher
blocklength
which have smaller trace than someof the gj.
LEMMA 3. Let W be a reduced
positive
!7-word and ij
beintegers,
thentr(g W) tr(gj W).
Thehyperbolic
elementof
smallest traceof
blocklength
1 is
gl-11g2.
Proof.
LetWe use
induction,
hence we prove the first statementwith j replaced by
i + 1.
Since ai
=di
for all i, it is sufficient to prove that ai + 1 > ai,bi + 1 > bi
and ci + 1 > ci.
However, ai
> ci is shown in[S-S],
and since ai + 1 =bi
andci+1 = ai’ we are done. The second statement follows
directly
from thefirst note that the element
yl-11h2
also has this trace.EXAMPLE. The shortest
geodesics
when = 4.The shortest
geodesic
is theboundary geodesic,
as U is of trace À.Now, tr(g2)
= 2À andtr(g 3)
= 2Â2 - 2. Considergl1g2,
which is of trace(1
+2)03BB.
This trace is less than that of g2 whenever 1
2Â2 - 2/ À.
We also consider the trace for g3 and so on, as well as words inboth gi
andhj.
Inparticular
of these
latter,
one hastr(gn1hm1)
= nmÂ2 + 2.Thus when =
4, using
that thelength
of thegeodesic corresponding
toa
hyperbolic
of trace t is 2log(t
+~t2-4)/2
we obtain Table 1.Of course, the first
eight hyperbolics
as labeled remain the firsteight
shortest
geodesics
for anyG ¡ BJe
with > 4. Thatis,
the initiallength ordering
ofgeodesics
iseventually
stable asexpressions
in 03BB under thecontinuous deformation of
increasing
03BB.(See
below for thesignificance
ofinitial
ordering switches.)
The final two entries of Table 1
give
two distinctgeodesics
of the samelength.
We intend to discussmultiplicity (and intersection) phenomena
to greater detail inforthcoming
work. Here we willjust
remark thatlength
spectrummultiplicity
for our one-parameterfamily
of surfaces arises in each of two ways. Thefirst,
where the tracepolynomials
ofnon-conjugate hyperbolics
areidentical,
may bethought
of as structural2013thisphenom-
enon exists even for the
0393q.
Inaddition,
as 03BBincreases,
size order of two traces may reverse. As À is a continuousvariable,
there will be an(algebraic)
value for which the traces are identical. This sort ofmultiplicity
may be
thought
of as accidental.(These
twospecies
ofmultiplicity
exist onmany families of
surfaces;
ourpoint
is that the Hecke surfaces arealready
complex enough
to exhibitboth.)
Table 1. The shortest geodesics, = 4
Table 2. Accidental multiplicity
To illustrate this
phenomenon,
we offer Table2,
in which we show thetrace of a
primitive hyperbolics fixing
lifts of each of twogeodesics
and thelength
of thesegeodesics
as functions of 03BB as well asgive
anexpansion
tofirst order terms of the real deformation variable 8 in a
neighborhood
ofÀ = 4
(the place
where both traces are68,
ofcourse).
As Buser notes
[Bu, p. 273],
oftensurprisingly
small initialportions
ofthe
length spectrum
serve as moduli for a surface. As the notationindicates,
G03BBBH
is determinedby
one real parameter. It is notsurprising then,
thatthe
length
of theboundary geodesic
ofG03BBBH
also serves as a parameterdetermining
the surface(up
to Teichmüllerclass).
This may be seencanonically using
two facts:first,
viaSL(2, R) conjugation,
every surface withsignature (0; 2, ~;1) 2013sphere
with one puncture, oneelliptic
fixedpoint
of order2,
and onehole may
berepresented by
a Fuchsian groupwith an
elliptic
elementfixing
i and aparabolic
elementfixing
00. It willthus have the usual fundamental
region
Hecketriangle
group of infinitevolume; i.e.,
boundedby
the unit circle and two vertical linesthrough
±
À/2. Second,
the formula for thehyperbolic fixing
the lift of theboundary geodesic
to this fundamentalregion given
in the next section.4. The Hall ray
We shall show
that,
ingeneral,
the Hecketriangle
groups possess a Hall ray. We take thegeometric
definition of a surfacepossessing
a Hall ray:there exists a real H such that for
any h
greater than H there aregeodesics
with
height arbitrarily
close to h. Theheight
of ageodesic
is thelargest
euclidean radius of any lift of the
geodesic
to H.(The
Hall ray is the rayrunning
from lim inf of such H and+00.)
The knownexamples
to date ofsurfaces with Hall rays are all related to the modular
surface,
see[H2].
Establishing
the existence of a Hall ray turns out to be easiest to prove for groups of the second kind with >J8. Using 03BBCF’s,
it is a routinematter to show that each of the Hecke groups of the first kind admits a
Hall ray. That
is,
theoriginal
Hall argumentapplicable
to the modularsurface,
can be extended to all finite volume Hecke groups. Thegeometric
issues in the first kind and second kind cases are
similar;
wegive
theproof
of the first kind case for
completeness.
4.1 The Hall ray
for G03BB
with  = 2 cosn/q
The naive
height
of a lift to the Poincaré upperhalf-plane
of ageodesic
ona Riemann surface with a
single
cusp is the euclidean diameter of this lift.The
height
of ageodesic
is the lim sup of the naiveheights
of all lifts of thisgeodesic.
The Cohn-Markoff spectrum is the set of allheights
ofgeodesics
of the surface. If the Cohn-Markoff spectrum of a surface contains a ray of
values,
the surface is said to have a Hall ray. In the literature todate,
allsurfaces known to have a Hall ray are
(commensurate with) coverings
ofthe modular surface. We show that
for q
>4, G qadmits
a Hall ray, withall values greater than or
equal
to p =603BBq being
included in the ray. Since A. Haas[H2]
has shown that the caseof q
= 4 follows from the existenceof the classical Hall ray
for q
=3,
our resultimplies
that everyGq
has aHall ray.
Our
proof is
anadaptation
of Hall’soriginal,
aspresented
in[C-F].
Wethank A. Haas for
pointing
out an error in ouroriginal proof.
Thedetermination of the
precise beginning
value of the Hall ray forG3
isnotoriously
difficult. Here weonly identify
a lower boundbeyond
whichthe ray extends.
One cannot use continued fraction
expansions
for theG qwhich
involveonly positive signs,
as in theordinary
continued fractions of the classicalsetting.
Here we use the nextfractions,
as in[S-S].
The crucialadvantage
in the
present setting
over the use of the otheroption,
the Rosen 03BB continuedfractions,
is thesimple
detection of the naturalordering
of thereals.
The next fractions are
given by
use ofpositive partial quotients,
butonly negative signs
between.Thus,
we use thesymbol
where all
ai,i > 0
arepositive integers; by
mild abuse ofnotation,
we willrefer to
the ai
as thepartial quotients
of such anexpansion.
In thisform,
03BBq itself
has aperiodic expansion:
where we use an overline to indicate a
period,
andln
to represent astring
of n consecutive l’s. The
period of  q
indicates the maximal number of consecutive l’s which appear in any(reduced)
next fraction.It is
known,
see say[S-S],
that every real can beexpanded
in a nextfraction. Thus
given
a lift of ageodesic
on the surfaceGqBH,
the feet of any of its lifts can beexpanded
out in such continued fractions. Of course, any translation of this lift will have the same naiveheight.
Thus we may normalize lifts so as to consider those with one foot between 0and
andthe other greater than
03BBq.
Thelarger
foot will haveexpansion fi
=[ao; a1, ... ],
while the smaller will be a = -[0;
a - 1, a -2,...].
Since theexpansion
of the formercorresponds
to theimage
ofinfinity
undersaOTsalT...,
it iseasily
seen that TS-’l takes this to[a1; a2, ...]
whilesending
the other footto -[0;a0, a-1,...].
Since the diameter of theoriginal
lift isit is clear that the set of the lim sup of all such sums for allowable double sequences of
the ai
is the same as the Cohn-Markoff spectrum ofGq.
THEOREM.
Let q
> 4.Any
real number greater than603BBq is
contained in theMarkoff
spectrumof Gq .
We use the
following
two lemmas.LEMMA 4.
Let q
> 4.Any
real number can be written inthe form
where a is an
integer
and theb,
and ci do not exceed 7.This follows from
LEMMA 5.
Let q
> 4.Any
real number in the intervalcan be written in the
form
where a is an
integer
and theb,
and ci do not exceed 7.Let
F(k)
be the set of real numbers a such that the next fraction of a has nopartial quotient larger
than kand -103BBq ~
a~ 1/[].
Of course, Lemma 2 isequivalent
toTo prove the above
equation by [C-F;
pp.47-51],
we needonly
showthat
F(7)
is obtainedby
a Cantor dissection process for which each interval removed is smaller than either of the subintervals createdby
its removal.Our deletion process has a
single
rule: from an intervalwhere 2 ~ m ~ k and W = w 1, w2, ... , 1 w. is of
minimal length
we removeIt is
easily
verified that after all(the countably many) applications
of thisrule to
exactly F(k)
remains. Inpractice, k
will beequal
to7;
W will consist of consecutivepartial quotients
from1q-3, 2;
and W must not end with 1 asa
partial quotient.
We now show that
for k ~
7 thelengths
of each excised interval is shorter than that of either of the subintervals which this excision creates.We label:
Note that
Thus we let
We now call
[k] simply
K. Basic continued fractionformuli, analogous
to[CF; (9)], give
If
r+1/r+1 = [0;a1, ... ar,m],
thenr+ 1
= Pr+1 +03BBqpr
andsimilarly
for the denominators. Thus
We must show that
This last
equation
isequivalent
toNow,
This last
equation
is bounded aboveby 03BBq,
because our excision rule dictates that m - 1 ~ 1 and that there can be at most q - 3 consecutive l’s in the sequencem - 1,
a,, ar-1,...,a1. Theright-hand
side is atmost Âq
and if K à
6À-q,
we are done.We now show that
|M1| ~ |I|.
Let co =[W,1q-3,2].
ThusIt suffices to show that
But, 2Âq
> co; hence if x >4À.q,
thenThus Ka
6Âq
suffices for this part as well. Inconclusion,
if k = 7 thenany of the removed intervals is shorter than either of the subintervals which its removal causes.
We now prove our theorem. From the
above,
This interval has
length
greater thanÀ-q,
hence we may express any 03BC ~6Âq
as
where a ~ 8 and
bi ~ 7,
c, ~ 7. Letwhich is say
[ao;
al, a2’...],
wherek,
is astrictly increasing
sequence ofintegers.
From our definition of thespectrum
for these continuedfractions,
it is clear that the
spectral
value for a is indeed M.Since the cover of
GqBH corresponding
to the commutatorsubgroup
ofGq
can be shown to be of genus(q - 1)/2
and of asingle
cuspif q
is odd(a
similar formula holds for even q, but then one has twocusps),
argumentsas in
[H2] (but
without use ofMillington’s theorem)
show thatCOROLLARY. For every genus g, there is a Riemann
surface
with asingle
cusp which admits a Hall ray.
REMARKS.
First,
a mostvexing question concerning
the classical Markoff spectrum deals with themysterious portion lying
below the Hall ray and above3,
the limitpoint
of the discrete part. We have noinsight
intowhether or not an
analogous portion
exists in the case of the Hecke groups.But we can say that a discrete
portion
does exist. This follows from the construction of lowheight geodesics given
in[S].
Second,
the observant reader may think that a step or two of the aboveproof
seemsoverly
cautious. Wepoint
out here that theapproximants pi/qi
for a next fraction can
display
amildly perturbing phenomenon.
Infact,
it can
happen that qi
> qi + 1. Of course, this neverhappens
for theordinary
continued
fractions,
and[R]
showed that it neverhappens
for the RosenÀ fractions. We
give
anexample:
Let q
= 5 and consider theapproximants
to[1, m, 1, 1, ... ],
with m ~ 2.Here q2 = mÀs
+ m - 1 which isclearly
greater than q3 =(m - 1)03BB5
+ m.One
might
now be concerned about the convergence of the next fractions to the reals whichthey
represent, but it iseasily
checked that theqi are
increasing
unless apartial
denominator is 1 and when astring
ofconsecutive l’s
ends,
then the next qi +n must in fact belarger.
This allows convergenceproofs
to gothrough.
4.2 The Hall ray
for GÂ
with  >fi
Let JV be the Nielsen convex
region
ofGÀ.
This isgiven by cutting
off thefunnel in the standard fundamental
region by
acircle, W, perpendicular
toboth the unit circle
(U)
and the line9t(z) = À/2.
It is easy to check that W has center at
À/2
and diameter~03BB2-
4(which
is
larger
than2).
Thepoint
of intersection of W with 4Y is(2/Â, ~1- 4/ À. 2);
that with the line
9i(z) = À/2
is(03BB/2, ~03BB2/4-1). (In
theSFR,
the entiregeodesic
iscomprised
of the arc between these twopoints
and acompanion
which is the reflection of this arc
by
z~ -.)
The
projection
of W toG ¡ B:K
is(infinitely
manycopies of)
theboundary geodesic.
The diameter of Walong
9iis,
apart from itsendpoints
which arelimit
points (hyperbolic
fixedpoints
since theboundary geodesic
isclosed in
fact, they
are fixedby
a matrix which is
(crucially) elliptic
if 03BB2!), comprised
of adoubly
infinitesequence of free sides. Likewise for the translates
by S ¡
of this diameter.These translates take up the entire real
axis,
apart from intervals oflength
less than 2. These intervals contain all limit
points,
of course. Take aheight
greater than 1. Draw an h-line of this naiveheight.
This line may be slidalong
the real axis so that both its feet lie in the free sideamalgamations.
(The
first set ofintervals.)
It is clear that the naive
height
of thisgeodesic
is its trueheight
as theentire
portion
of thegeodesic
outside translates of the SFR liesbeyond
theboundary geodesic.
Thisgeodesic
has two infinite ends2013it is not closed in either direction.What if we
require
thegeodesics
we consider to be closed? If we restrictour attention to closed
geodesics,
then there may be no Hall ray. This iseasily
illustrated as follows:Assume À is
large,
100 say, then all closedgeodesics
have feet inAny geodesic
ofheight h,
for 2 + 50n h 48 +50n;
n ~ Z cannot haveboth feet in 5. Thus there is no Hall ray for closed
geodesics.
We see thatthe notions of
Markoff spectrum (a
closedgeodesic infinite
03BBCFphenom- enon)
and Cohn spectrum(a geodesic height phenomenon)
have bifurcated in this context.Acknowledgements
T. A. Schmidt thanks Alf van der Poorten and
Macquarie University,
where this work was
initiated;
WidenerUniversity
for generousgranting
ofleaves of
absence;
and the NSF-RUI program. M.Sheingorn
thanks theNSF and PSC-CUNY for
supporting
this research.References
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