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Luca De Feo
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Small correction, thank you, Ryan
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poly.tex

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@@ -81,6 +81,7 @@
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\DeclareMathOperator{\im}{Im} % imaginary part
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\DeclareMathOperator{\re}{Re} % real part
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\DeclareMathOperator{\GL}{GL}
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\DeclareMathOperator{\PGL}{PGL}
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\DeclareMathOperator{\SL}{SL}
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\DeclareMathOperator{\Cl}{Cl}
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\DeclareMathOperator{\Ell}{Ell}
@@ -218,8 +219,8 @@ \section*{Preface}
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fixing them. %
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We would like to thank, in particular, Simon Masson, Marcel Müller,
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Martin Strand, Vadym Fedyukovych, Tomáš Novotny, Sina Schaeffler,
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Val\'erien Hatey, Mehdi Kermaoui, and apologize to all those students
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whose name we've forgot.
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Val\'erien Hatey, Mehdi Kermaoui, Ryan Rueger, and apologize to all
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those students whose name we've forgot.
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\clearpage
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{
@@ -2045,8 +2046,9 @@ \section{Isogeny volcanoes}
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Remark that being $$-isogenous is also well defined up to
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isomorphism.
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Let us start from the local structure: given an elliptic curve $E$ and
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a prime $$, how many isogenies of degree $$ have $E$ as domain? %
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Let us start with the local structure of the graph: given an elliptic
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curve $E$ and a prime $$, how many isogenies of degree $$ have $E$
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as domain? %
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Thanks to Proposition~\ref{prop:isoker}, we know this is equivalent to
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asking how many subgroups of order $$ the curve has; but then we
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immediately know there are exactly $ℓ+1$ isogenies whenever $ℓ≠p$.
@@ -2098,9 +2100,10 @@ \section{Isogeny volcanoes}
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to $E[ℓ]$. %
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Assume $ℓ≠p$, then $E[ℓ]$ is a group of rank $2$ and $π$ acts on it
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like an element of $\GL_2(\F_ℓ)$, up to conjugation. %
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Clearly, the order of $π$ in $\GL_2(\F_ℓ)$ is the degree of the
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smallest extension of $\F_q$ where all $$-isogenies of $E$ are
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defined. %
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If $n$ is the smallest exponent such that $π^n$ acts like a scalar
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multiplication, i.e.\ if $n$ is the order of $π$ in $\PGL_2(\F_ℓ)$,
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then $\F_{q^n}$ is the smallest field where all $$-isogenies of $E$
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are defined. %
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But we can tell even more by diagonalizing the matrix: $π$ must have
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between $0$ and $2$ eigenvalues, and the corresponding eigenvectors
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define kernels of rational isogenies. %
@@ -2129,7 +2132,7 @@ \section{Isogeny volcanoes}
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factorization of its characteristic polynomial $x^2-tx+q$ over $\F_ℓ$,
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or equivalently on whether $Δ_π=t^2-4q$ is a square modulo $$. %
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But what about the global structure? %
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But what about the global structure of the graph? %
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Any curve $E/\F_q$ can be seen as the reduction modulo $p$ of some
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curve $E/\bar{ℚ}$; thus it must inherit the connectivity structure of
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the isogeny graph of $E/\bar{ℚ}$. %

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