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HyperGeography and SuperHyperGeography

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02 October 2025

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03 October 2025

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Abstract
A Hyperstructure is built on the concept of the powerset, providing a framework to model interactions among elements of a set. Extending this concept, a Superhyperstructure employs the n-th powerset to represent hierarchical systems with multiple layers, enabling richer abstractions and more complex relationships. Geography is a mathematical framework on a 2D Riemannian manifold encoding regions, features, attributes, networks, and projections to analyze spatial relations. In this paper, we examine whether Hyperstructures and SuperHyperstructures can be employed to define HyperGeography and SuperHyperGeography, and we provide a concise discussion including potential applications.
Keywords: 
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1. Preliminaries

This section gathers the basic notions and notation used throughout the paper. Unless explicitly stated otherwise, we work in the finite setting. By convention, the empty set is treated as an element of every set.

1.1. Hyperstructure and Superhyperstructure

A Hyperstructure is organized around the powerset and serves as a vehicle for modeling relations among elements of a set [1,2,3,4,5,6]. Owing to its flexibility, the hyperstructure framework has been investigated across several areas, including mathematics and chemistry [7,8,9,10]. A Superhyperstructure advances this idea by utilizing the n-th powerset to encode multi-layered hierarchical interactions, thereby enabling deeper abstraction and greater structural complexity [11,12,13]. Related concepts such as SuperHyperGraph are also known [14,15,16,17,18]. We next record the n-th powerset, which underpins these structures.
Definition 1
(Base Set). A base set S is the underlying collection from which higher-level constructions—powersets and (super)hyperstructures—are built. Formally,
S = { x x is an element of a specified domain } .
All elements appearing in P ( S ) or in the iterated powersets P n ( S ) ultimately arise from members of S.
Definition 2
(Powerset). [19] The powerset of a set S, denoted P ( S ) , is the family of all subsets of S, including ∅ and S itself:
P ( S ) = { A A S } .
Example 1
(Powerset in a geographic partition). Let S = { N , S , C } denote three disjoint administrative regions of a city: North ( N ) , South ( S ) , and Coast ( C ) . The powerset
P ( S ) = { , { N } , { S } , { C } , { N , S } , { N , C } , { S , C } , { N , S , C } }
contains 2 | S | = 2 3 = 8 subsets. Suppose their areas are
μ ( N ) = 30 km 2 , μ ( S ) = 25 km 2 , μ ( C ) = 20 km 2 .
For any A S , the union A represents the geographic footprint of the chosen regions (with = and μ ( ) = 0 ). For instance,
A = { N , C } A = N C , μ ( N C ) = μ ( N ) + μ ( C ) = 30 + 20 = 50 km 2 ,
since the regions are disjoint. This concretely interprets P ( S ) as all possible selections of regions for a planning scenario.
Definition 3
(n-th Powerset). (cf.[20,21,22,23]) For a set H, the n-th powerset P n ( H ) is defined recursively by
P 1 ( H ) = P ( H ) , P n + 1 ( H ) = P P n ( H ) , n 1 .
The nonempty version P n * ( H ) is given by
P 1 * ( H ) = P * ( H ) , P n + 1 * ( H ) = P * P n * ( H ) ,
where P * ( H ) = P ( H ) { } .
Example 2
(n-th powerset (here n = 2 ) for district portfolios). Let H = { D 1 , D 2 , D 3 } be three disjoint districts with areas
μ ( D 1 ) = 12 km 2 , μ ( D 2 ) = 9 km 2 , μ ( D 3 ) = 5 km 2 .
Then
P 1 ( H ) = P ( H ) has cardinality 2 3 = 8 , P 2 ( H ) = P P 1 ( H ) has cardinality 2 8 = 256 .
For the nonempty versions, P 1 * ( H ) = P ( H ) { } has 2 3 1 = 7 elements, hence
P 2 * ( H ) = P * ( P 1 * ( H ) ) = 2 7 1 = 127 .
A concrete element of P 2 * ( H ) (a nonempty set of nonempty district-sets) is
X = { D 1 , D 2 } , { D 2 } , { D 3 } P 2 * ( H ) .
Its geographic coverage is the union of all districts that appear in X:
X = D 1 D 2 D 3 , μ ( D 1 D 2 D 3 ) = 12 + 9 + 5 = 26 km 2 .
Thus, P 2 ( H ) parameterizes portfolios of district groupings (e.g., policy or service bundles), while P 2 * ( H ) restricts to portfolios with no empty members.
To provide a self-contained foundation for hyperstructures and superhyperstructures, we recall the following standard notions.
Definition 4
(Classical Structure). (cf. [20,21,24]) A Classical Structure consists of a nonempty set H together with one or more classical operations satisfying specified axioms. A classical m-ary operation has the form
# 0 : H m H ,
with m 1 . Familiar examples include the operations defining groups, rings, and fields.
Definition 5
(Hyperoperation). (cf. [11,25,26,27]) A hyperoperation on a set S is a map
: S × S P ( S ) ,
so that combining two inputs returns a set of outcomes (not necessarily a singleton).
Definition 6
(Hyperstructure). (cf. [20,21,28,29]) A Hyperstructure augments a base set S by operating on its powerset. Formally,
H = ( P ( S ) , ) ,
where ∘ acts on subsets of S.
Example 3
(HyperStructure — capacity–constrained parcel consolidation). Let the base set be parcels S = { a , b , c , d } with weights (kg)
w ( a ) = 3 , w ( b ) = 4 , w ( c ) = 5 , w ( d ) = 6 ,
and let the vehicle capacity be C = 10 kg. Consider the HyperStructure
H = P ( S ) , cap ,
where the hyperoperation cap : P ( S ) × P ( S ) P P ( S ) { } maps two order sets X , Y S to the set of all feasible trip partitions Z such that: (i) Z = X Y , (ii) for every T Z one has x T w ( x ) C .
Take X = { a , b } and Y = { c } . Then X Y = { a , b , c } with total weight 3 + 4 + 5 = 12 > 10 , so at least two trips are needed. Enumerating all set partitions of { a , b , c } and keeping only capacity–feasible ones gives
{ a , b } , { c } : 3 + 4 = 7 10 , 5 10 ; { a , c } , { b } : 3 + 5 = 8 10 , 4 10 ;
{ b , c } , { a } : 4 + 5 = 9 10 , 3 10 ; { a } , { b } , { c } : 3 , 4 , 5 10 .
The single–trip partition { { a , b , c } } is infeasible since 12 > 10 . Therefore
X cap Y = { { a , b } , { c } } , { { a , c } , { b } } , { { b , c } , { a } } , { { a } , { b } , { c } } ,
illustrating a concrete hyperoperation on P ( S ) returning multiple feasible consolidation outcomes under a real capacity constraint.
Definition 7
(SuperHyperOperation). [20] Let H be nonempty. Define recursively, for k 0 ,
P 0 ( H ) = H , P k + 1 ( H ) = P P k ( H ) .
For fixed m , n 0 and arity s 1 , an ( m , n ) -SuperHyperOperation is a map
( m , n ) : P m ( H ) s P n ( H ) .
If the codomain may include ∅, we obtain the neutrosophic variant; otherwise we are in the classical case.
Definition 8
(n-Superhyperstructure). (cf. [20,23,30,31]) An n-Superhyperstructure generalizes hyperstructures by acting on the n-th powerset:
SH n = ( P n ( S ) , ) ,
with ∘ defined on P n ( S ) .
Example 4
(n-Superhyperstructure ( n = 2 )—team reorganization with size constraints). Let S = { e 1 , e 2 , e 3 , e 4 , e 5 , e 6 } be employees. A level–2 object X P 2 ( S ) = P ( P ( S ) ) is a set of teams (each team is a nonempty subset of S). Define an operation
team : P 2 ( S ) × P 2 ( S ) P P 2 ( S ) { }
that maps programs X , Y to the set of all reorganizations Z whose ground union is preserved and whose teams have size in { 2 , 3 } (no singletons):
Z = ( X Y ) S , T Z : 2 | T | 3 .
Take
X = { e 1 , e 2 } , { e 3 } , Y = { e 4 , e 5 } , { e 6 } .
Then ( X Y ) = { e 1 , , e 6 } . Two canonical families in X team Y are:
Z triads = { e 1 , e 2 , e 3 } , { e 4 , e 5 , e 6 } , Z pairs = { e 1 , e 4 } , { e 2 , e 5 } , { e 3 , e 6 } .
Counting shows the operation returns many outcomes: the number of partitions of six labeled employees into two unlabeled triads is
1 2 6 3 = 1 2 · 20 = 10 ,
and the number of partitions into three pairs (perfect matchings) is
( 6 1 ) ! ! = 5 ! ! = 15 .
Hence X team Y contains at least 10 + 15 = 25 reorganizations satisfying the size constraint, which demonstrates a concrete n-Superhyperstructure on P 2 ( S ) producing multiple valid teamings while preserving the same ground set.
Definition 9
(SuperHyperStructure of order ( m , n ) ). (cf. [11,32,33]) Let S be nonempty and m , n 0 . A ( m , n ) -SuperHyperStructure of arity s is any choice of
( m , n ) : P m ( S ) s P n ( S ) .
The special cases recover standard settings: m = n = 0 gives ordinary s-ary operations; m = 0 , n = 1 yields hyperoperations; and s = 1 corresponds to superhyperfunctions.
Example 5
( ( m , n ) -SuperHyperStructure with ( m , n ) = ( 2 , 1 ) — two–layer service bundles to single–layer deployment). Let S = { A 1 , A 2 , A 3 , A 4 } be neighborhoods with areas (km2)
μ ( A 1 ) = 8 , μ ( A 2 ) = 5 , μ ( A 3 ) = 6 , μ ( A 4 ) = 7 ,
and population densities (persons/km2)
ρ ( A 1 ) = 7 , 000 , ρ ( A 2 ) = 6 , 000 , ρ ( A 3 ) = 3 , 500 , ρ ( A 4 ) = 2 , 000 .
Thus atomic populations are
P ( A 1 ) = 8 × 7 , 000 = 56 , 000 , P ( A 2 ) = 5 × 6 , 000 = 30 , 000 ,
P ( A 3 ) = 6 × 3 , 500 = 21 , 000 , P ( A 4 ) = 7 × 2 , 000 = 14 , 000 ,
and over S one has
P ( S ) = 56 , 000 + 30 , 000 + 21 , 000 + 14 , 000 = 121 , 000
and total area 8 + 5 + 6 + 7 = 26 km2, hence the average density on the union is
ρ ¯ = 121 , 000 26 4 , 653.846 persons / km 2 .
A level–2 bundle is an element of P 2 ( S ) . Consider two agencies’ proposals
X = { A 1 , A 2 } , { A 3 } , Y = { A 4 } .
Define the ( 2 , 1 ) -superhyperoperation
( 2 , 1 ) : P 2 ( S ) × P 2 ( S ) P P ( S ) { }
by
X ( 2 , 1 ) Y : = Z P ( S ) { } : Z = X Y .
A canonical output is the flattened selection
Z 0 = { A 1 , A 2 , A 3 , A 4 } X ( 2 , 1 ) Y ,
and any other Z in the output has the same ground union. If each person needs r = 0.05 kits/month, the single–layer monthly demand is
D = r · P ( S ) = 0.05 × 121 , 000 = 6 , 050 kits / month ,
which is invariant across all Z X ( 2 , 1 ) Y because it depends only on the flattened union. This realizes a concrete ( m , n ) -SuperHyperStructure with ( m , n ) = ( 2 , 1 ) : inputs at level 2 (bundles) and outputs at level 1 (deployable region selections) while preserving measurable aggregates.

2. Main Results

In this section, we present the main contributions of this paper.

2.1. Geography

Geography is a mathematical framework on a 2D Riemannian manifold encoding regions, features, attributes, networks, and projections to analyze spatial relations [34,35,36,37,38,39].
Definition 10
(Geography as a mathematical structure). (cf.[40,41]) Fix a nonempty, connected, oriented 2-dimensional C 1 manifold M (the ground) endowed with a Riemannian metric g. Let
d : = d g be the induced geodesic distance , μ : = H g 2 the induced Borel area measure ,
and let Σ be the Borel σ-algebra on M. A geography is a tuple
Geo = ( M , g , d , μ , Σ , P , F , A , att , N , proj )
satisfying the axioms (G1)–(G6) below.
(G1) Regions (administrative/physical partition).  P = { R i } i I Σ is a countable family of pairwise μ-almost disjoint measurable sets with
μ M i I R i = 0 , H g 1 ( R i ) < for all i I .
For R , S P with R S , define adjacency
R S : H g 1 R S > 0 .
(G2) Features (typed geometric objects). F is a set of triples f = ( S f , dim f , α f ) where S f M is a countably H g dim f -rectifiable set of finite H g dim f -measure, dim f { 0 , 1 , 2 } , and α f : S f V f is a measurable attribute map into a measurable space ( V f , B f ) . Conventionally, dim f = 0 (points, e.g. cities), 1 (curves, e.g. rivers/roads), or 2 (areas, e.g. lakes/parks).
(G3) Attribute fields (spatial variables).  A is a (finite or countable) index set. For each a A there is a measurable value space ( V a , B a ) and a measurable field
A a : ( M , Σ ) ( V a , B a ) , written att ( a ) = A a .
Numerical fields satisfy A a L loc 1 ( M , μ ) ; for such a and any E Σ of finite μ-measure, define the aggregate
Agg a ( E ) : = E A a d μ .
(G4) Embedded networks (transport/flow).  N = ( G , φ ) where G = ( V , E ) is a (finite or countable) simple graph and φ embeds G into M via
φ V : V M , φ E : E { rectifiable curves in M } ,
so that each e = { u , v } E is mapped to a rectifiable curve φ E ( e ) whose endpoints are φ V ( u ) , φ V ( v ) . The network length measure ℓ is the 1-dimensional Hausdorff measure restricted to e E φ E ( e ) .
(G5) Spatial relations.  From (G1)–(G4) derive measurable binary relations on regions/features, e.g.
R touches S : H g 1 ( R S ) > 0 , R contains S : μ ( S R ) = 0 , dist ( E , F ) : = inf { d ( x , y ) : x E , y F } ,
for measurable E , F M . These are well-defined because d is a metric and μ , H g k are Borel regular.
(G6) Coordinate realization / projection (cartography).  proj is an optional specification of coordinates: either a chart π : M S 2 (reference ellipsoid/sphere) or a locally C 1 map P : M R 2 (a cartographic projection) which is a local diffeomorphism off a set of μ-measure 0.
Remark 1
(Minimal consequences). For any finite subpartition { R i } i = 1 n P with μ M i = 1 n R i = 0 , σ-additivity yields the exact decomposition
μ ( M ) = i = 1 n μ ( R i ) .
For any integrable numerical attribute A a L 1 ( M , μ ) ,
M A a d μ = i = 1 n R i A a d μ ,
and for regions R S one has
dist ( R , S ) = 0 H g 1 ( R S ) > 0 ,
so adjacency R S implies dist ( R , S ) = 0 , while dist ( R , S ) > 0 implies non-adjacency.
Example 6
(Urban water supply and mobility planning). We instantiate Geo on a metropolitan area.
(G1) Ground and regions. Let M R 2 be a bounded open set with smooth boundary, endowed with the Euclidean metric g = Id . Let Σ be the Borel σ-algebra and μ the Lebesgue area measure (so μ is the 2-dimensional Hausdorff measure). Partition M into three measurable regions (almost disjoint, finite perimeter)
P = { R 1 , R 2 , R 3 } , μ ( R 1 ) = 40 km 2 , μ ( R 2 ) = 25 km 2 , μ ( R 3 ) = 15 km 2 ,
with adjacencies R 1 R 2 , R 1 R 3 , and dist ( R 2 , R 3 ) > 0 (separated by a river corridor).
(G2) Features. Let F contain: (i) a curve feature f river = ( S riv , 1 , α riv ) where S riv is a rectifiable river centerline crossing R 1 and separating R 2 from R 3 ; (ii) point features f res , k = ( { p k } , 0 , α res , k ) for reservoirs p k with storage attribute α res , k ( p k ) R + ; (iii) area features f park , j = ( S park , j , 2 , α park , j ) for urban parks.
(G3) Attribute fields. Define population density and monthly rainfall fields
A pop ( x ) = 10 , 000 x R 1 , 7 , 000 x R 2 , 3 , 000 x R 3 , A rain ( x ) = 180 x R 1 , 160 x R 2 , 150 x R 3 ,
measured in persons / km 2 and mm / month , respectively. Then the regional populations are
Agg pop ( R i ) = R i A pop d μ = density i · μ ( R i ) ,
so numerically
Pop ( R 1 ) = 10 , 000 × 40 = 400 , 000 , Pop ( R 2 ) = 7 , 000 × 25 = 175 , 000 , Pop ( R 3 ) = 3 , 000 × 15 = 45 , 000 , Pop ( M ) = 620 , 000 .
Monthly rainfall volume over R i (assuming spatially constant per region) is
V rain ( R i ) = A rain ( R i ) 1000 · μ ( R i ) × 10 6 m 3 ,
since 1 km 2 = 10 6 m 2 . Hence
V rain ( R 1 ) = 0.18 × 40 × 10 6 = 7.2 × 10 6 m 3 , V rain ( R 2 ) = 0.16 × 25 × 10 6 = 4.0 × 10 6 m 3 , V rain ( R 3 ) = 0.15 × 15 × 10 6 = 2.25 × 10 6 m 3 .
(G4) Embedded networks. Let G = ( V , E ) be the primary road graph with major hubs V = { v 1 , v 2 , v 3 } (one per region) and edges E = { { v 1 , v 2 } , { v 1 , v 3 } , { v 2 , v 3 } } . Embed each edge as a rectifiable curve φ E ( e ) M with lengths
φ E ( { v 1 , v 2 } ) = 12 km , φ E ( { v 1 , v 3 } ) = 10 km , φ E ( { v 2 , v 3 } ) = 8 km .
The total embedded edge length is ( e E φ E ( e ) ) = 30 km (edges disjoint except at endpoints).
(G5) Spatial relations. By construction, R 1 R 2 and R 1 R 3 since H g 1 ( R 1 R i ) > 0 for i = 2 , 3 , while dist ( R 2 , R 3 ) > 0 (the river corridor enforces a positive gap).
(G6) Projection. Take P : M R 2 to be the local UTM projection (chart on the chosen zone); P is C 1 and a local diffeomorphism off a null set, enabling planar cartography.
This instantiation supports concrete planning queries such as allocating stormwater storage to match { V rain ( R i ) } i = 1 3 and sizing road capacities along φ E to serve { Pop ( R i ) } .
Example 7
(Coastal evacuation and shelter capacity). We instantiate Geo on a coastal city with tsunami hazard zoning.
(G1) Ground and regions. Let M R 2 be a simply connected coastal municipality with Euclidean metric g, Borel σ-algebra Σ, and Lebesgue area measure μ. Partition M into hazard/land-use regions
P = { H 1 , H 2 , H 3 } , μ ( H 1 ) = 12 km 2 , μ ( H 2 ) = 28 km 2 , μ ( H 3 ) = 10 km 2 ,
where H 1 is the tsunami inundation zone (low elevation), H 2 is inland residential, and H 3 is an industrial port. Assume H 1 H 2 , H 1 H 3 , and dist ( H 2 , H 3 ) > 0 .
(G2) Features. Include: (i) shoreline curve f shore = ( S shore , 1 , α shore ) with α shore carrying local berm height; (ii) evacuation shelters as point features f sh , k = ( { q k } , 0 , α cap , k ) with capacities α cap , 1 ( q 1 ) = 60 , 000 , α cap , 2 ( q 2 ) = 50 , 000 , α cap , 3 ( q 3 ) = 30 , 000 ; (iii) critical bridges as curve features with width attributes.
(G3) Attribute fields. Define elevation (meters above sea level) and population density
A elev ( x ) = 2 x H 1 , 12 x H 2 , 4 x H 3 , A pop ( x ) = 8 , 000 x H 1 , 6 , 000 x H 2 , 1 , 500 x H 3 ,
in m and persons / km 2 . Then regional populations are
Pop ( H 1 ) = H 1 A pop d μ = 8 , 000 × 12 = 96 , 000 , Pop ( H 2 ) = 6 , 000 × 28 = 168 , 000 , Pop ( H 3 ) = 1 , 500 × 10 = 15 , 000 , Pop ( M ) = 279 , 000 .
Suppose the evacuation target is all residents in H 1 . Total designated shelter capacity is
Cap tot = k = 1 3 α cap , k ( q k ) = 140 , 000 Cap tot Pop ( H 1 ) = 44 , 000 ( sufficient by 44,000 ) .
(G4) Embedded evacuation network. Let G = ( V , E ) with V = { u 1 , u 2 , u 3 } representing the centroids of H 1 , H 2 , H 3 and with edges along designated evacuation corridors:
φ E ( { u 1 , u 2 } ) = 5.0 km , φ E ( { u 1 , u 3 } ) = 4.2 km , φ E ( { u 2 , u 3 } ) = 3.0 km .
The total corridor length is 12.2 km . If a bridge feature on { u 1 , u 2 } has width w = 8 m and safe pedestrian flux J max = 1.5 persons / ( m · s ) , then the link’s peak throughput is
Q max = w · J max = 12 persons / s 43 , 200 persons / h ,
so in principle one such link can clear H 1 in about 96 , 000 / 43 , 200 2.22 h under steady flow (ignoring transients and routing constraints).
(G5) Spatial relations. Because Υ ( H 1 ) meets both Υ ( H 2 ) and Υ ( H 3 ) along positive-length arcs, H 1 H 2 and H 1 H 3 . Moreover, dist ( H 2 , H 3 ) > 0 implies non-adjacency between H 2 and H 3 .
(G6) Projection. Take P to be a conformal coastal chart (e.g. local Mercator/UTM); since P is C 1 and locally invertible away from a null set, lengths/areas are well-defined up to the standard Jacobian factors used in map production.
This instantiation quantifies (i) required shelter capacity relative to Pop ( H 1 ) and (ii) corridor throughput via embedded network geometry, enabling data-driven evacuation timing analyses.

2.2. HyperGeography

HyperGeography extends Geography by treating sets of atomic regions as hyperregions and using a hyperoperation to generate partitions of their union.
Definition 11
(HyperGeography). Fix a countable family S = { A j } j J Σ of atomic regions such that
μ M j J A j = 0 , μ ( A j ) > 0 , H g 1 ( A j ) < ,
and A i A j are μ-almost disjoint for i j . Set the hyperregion universe to be the nonempty powerset
R : = P * ( S ) = P ( S ) { } .
Define the region hyperoperation reg : R × R P ( R ) { } by
X reg Y : = Z R : Z = ( X Y ) and Z is a finite subfamily of S .
Equivalently,
X reg Y X Y and X reg Y P { A S : A ( X Y ) } { } .
(Thus X reg Y returns all finite admissible partitions of the geometric union ( X Y ) by atoms from S, including the coarse partition { ( X Y ) } whenever ( X Y ) S ; if not, the set { X Y } is still an element of R because X Y S .)
Let F denote the set of typed geometric features as in Definition 10(G2); we allow hyperattachment to hyperregions via measurable maps
α f : R P ( V f ) { } , α f ( X ) : = α f ( x ) : x X S f * .
For spatial attributes, let A be an index set and for each a A fix a measurable field A a : ( M , Σ ) ( V a , B a ) as in (G3). For numeric attributes take V a = R and assume A a L loc 1 ( M , μ ) . Define the attribute hypervaluation on hyperregions:
Agg a : R P ( R ) { } , Agg a ( X ) : = 1 μ ( E ) E A a d μ : E Σ , E X , μ ( E ) < .
(Other admissible weightings can be inserted; this simple choice suffices for our theorems.)
Define the hypernetwork N h = ( G h , φ h ) by taking G h = ( V h , E h ) with V h = R and
{ X , Y } E h H g 1 ( X ) ( Y ) > 0 ,
and embed G h in M by φ h ( X ) M chosen, e.g., as the μ-barycenter of X and edges mapped to rectifiable curves contained in a small tubular neighborhood of ( X ) ( Y ) .
A HyperGeography is the tuple
HGeo : = M , g , d , μ , Σ , S , R , reg , F , α , A , Agg , N h , proj .
Remark 2
(Well-definedness). (i) X reg Y because X Y R and X Y X reg Y . (ii) Agg a ( X ) is nonempty since μ ( X ) > 0 and we can choose any measurable E X with 0 < μ ( E ) < . (iii) E h is well-defined because ( X ) and ( Y ) have finite H g 1 -measure whenever X and Y are finite unions of finite-perimeter atoms.
Example 8
(Multi-district hospital catchment as a hyperregion). We build a concrete HyperGeography on a city partitioned into atomic districts.
Atoms and measure.  Let M R 2 be a bounded open set with Euclidean metric g, Borel σ-algebra Σ, and area measure μ. Fix the atomic family S = { A 1 , , A 5 } Σ with
μ ( A 1 ) = 12 , μ ( A 2 ) = 9 , μ ( A 3 ) = 5 , μ ( A 4 ) = 7 , μ ( A 5 ) = 10 ( in km 2 ) ,
finite-perimeter boundaries H g 1 ( A j ) < , and pairwise μ-almost disjoint interiors. Assume adjacencies
A 1 A 2 , A 2 A 3 , A 3 A 4 , A 4 A 5 , A 1 A 5 ,
and all other pairs non-adjacent.
Hyperregions and hyperoperation.  The hyperregion universe is R = P * ( S ) . Consider two (possibly disconnected) service catchments:
X = { A 1 , A 3 } , Y = { A 2 } .
Their union in the ground space is ( X Y ) = A 1 A 2 A 3 (area = 12 + 9 + 5 = 26 km2). By Definition 11,
X reg Y = Z R : Z = ( X Y ) , Z S finite { A 1 , A 2 , A 3 } ,
so the fine partition { A 1 , A 2 , A 3 } is a valid hyperselection; any other finite atom-cover of A 1 A 2 A 3 is also admissible.
Attributes and hypervaluation.  Let population density be piecewise constant (persons/km2):
A pop ( x ) = 8 , 000 x A 1 , 6 , 000 x A 2 , 4 , 500 x A 3 , 3 , 000 x A 4 , 2 , 000 x A 5 .
Then regional populations on the atoms are
Pop ( A 1 ) = 8 , 000 × 12 = 96 , 000 , Pop ( A 2 ) = 6 , 000 × 9 = 54 , 000 , Pop ( A 3 ) = 4 , 500 × 5 = 22 , 500 .
For the hyperregion X Y , the classical average density is
ρ ¯ pop ( X Y ) = ( X Y ) A pop d μ μ ( ( X Y ) ) = 96 , 000 + 54 , 000 + 22 , 500 26 = 172 , 500 26 6 , 634.615 persons / km 2 .
By Definition of Agg ,
Agg pop ( X Y ) = 1 μ ( E ) E A pop d μ : E A 1 A 2 A 3 [ 4 , 500 , 8 , 000 ] ,
since choosing E A 3 (resp. E A 1 ) realizes the lower (resp. upper) endpoint.
If the expected monthly visit rate is r = 0.05 visits/person/month, then the hyperregion’s total baseline demand is
D month = r · Pop ( A 1 ) + Pop ( A 2 ) + Pop ( A 3 ) = 0.05 × 172 , 500 = 8 , 625 .
This number is independent of the chosen hyperselection Z X reg Y because it depends only on the ground-space union ( X Y ) .
Hypernetwork.  Vertices are all hyperregions V h = R . In particular,
{ { A 1 } , { A 2 } } E h and { { A 2 } , { A 3 } } E h
since H g 1 ( A 1 A 2 ) > 0 and H g 1 ( A 2 A 3 ) > 0 . Thus a path { A 1 } { A 2 } { A 3 } exists within the hypernetwork, even though the service hyperregion X = { A 1 , A 3 } is disconnected in the ground space.
Example 9
(Renewable-energy siting across disjoint ridges). We model a wind-farm siting problem where a developer considers two separated ridges and a transmission corridor.
Atoms and adjacencies.  Let S = { A 2 , A 3 , A 4 , A 5 } with areas
μ ( A 2 ) = 14 , μ ( A 3 ) = 8 , μ ( A 4 ) = 9 , μ ( A 5 ) = 11 ( km 2 ) ,
and adjacencies A 2 A 3 , A 5 A 4 , all other pairs non-adjacent.
Hyperregions.  Let the candidate generation sites be the two ridges
X = { A 2 , A 5 } ,
and the supporting transmission/buffer corridor be
Y = { A 3 , A 4 } .
Then ( X Y ) = A 2 A 3 A 4 A 5 (area = 14 + 8 + 9 + 11 = 42 km2), and by Definition 11
X reg Y { A 2 , A 3 , A 4 , A 5 } ,
with all other finite atom-covers of the same union also admissible hyperselections.
Attributes and hypervaluation.  Define wind-energy density (MWh/km2/day) as
A wind ( x ) = 5.5 x A 2 , 0.0 x A 3 , 0.0 x A 4 , 4.8 x A 5 .
The average wind density over the generation hyperregion X is
ω ¯ ( X ) = 5.5 · 14 + 4.8 · 11 14 + 11 = 77.0 + 52.8 25 = 129.8 25 = 5.192 .
The corresponding daily potential on X is ω ¯ ( X ) · μ ( X ) = 5.192 × 25 = 129.8 MWh/day, and over a 30-day month this is 129.8 × 30 = 3 , 894 MWh.
By hypervaluation,
Agg wind ( X ) = 1 μ ( E ) E A wind d μ : E A 2 A 5 [ 4.8 , 5.5 ] ,
with endpoints realized by E A 5 and E A 2 , respectively. For the combined siting-and-corridor hyperregion X Y , the hypervaluation enlarges to
Agg wind ( X Y ) [ 0.0 , 5.5 ] ,
since one may choose E A 3 (or A 4 ) yielding zero average, showing how corridor inclusion affects averaged density though not the total potential restricted to X.
Hypernetwork and routing.  In the hypernetwork ( G h , φ h ) , the vertices { A 2 } and { A 3 } are adjacent, as are { A 5 } and { A 4 } ; thus any hyperselection Z X reg Y contains an embedded path from the generation atoms to the corridor atoms along shared positive-length boundaries, which represents feasible interconnections without leaving ( X Y ) .
Operation invariants. For all Z X reg Y , the ground-space union is fixed: Z = ( X Y ) . Hence any quantity expressible as an integral over ( X Y ) (e.g. land take, environmental footprint governed by a density field) is invariant under the choice of hyperselection Z. Only how the union is partitioned (e.g. for permitting or ownership) varies.
Theorem 1
(Region layer of HyperGeography is a HyperStructure). Let HGeo be as in Definition 11. Then
H reg : = R , reg
is a HyperStructure in the sense of the Definition.
Proof. 
By construction, R = P * ( S ) is nonempty. For any X , Y R , the set X reg Y is nonempty because X Y R and X Y X reg Y by definition. Moreover X reg Y R since every Z X reg Y is a nonempty finite subfamily of S. Hence reg is a hyperoperation on R , proving that ( R , reg ) is a HyperStructure. □
Definition 12
(Canonical embedding of regions). Given a Geography Geo as in Definition 10, set S : = P = { R i } i I (the measurable partition of M). Let R = P * ( S ) and reg as in Definition 11. Define the singleton embedding
ι : P R , ι ( R ) : = { R } .
Lemma 1
(Compatibility of union and hyperunion). For any R , S P one has
ι ( R ) reg ι ( S ) ι ( R ) ι ( S ) = { R , S } ,
and
ι ( R ) ι ( S ) = R S .
Proof. 
By Definition 11, X reg Y always contains X Y . Taking X = ι ( R ) and Y = ι ( S ) gives the first claim. The second identity holds because { R , S } = R S . □
Theorem 2
(HyperGeography generalizes Geography). Let Geo = ( M , g , d , μ , Σ , P , F , A , att , N , proj ) be a Geography. Construct HGeo from Geo by taking S : = P and defining R , reg , α , Agg and N h as in Definition 11. Then:
(a)
Region recovery. The map ι : P R in Definition 12 is injective and
ι ( R ) = R , R P .
(b)
Adjacency recovery. For R S ,
R S H g 1 ( ι ( R ) ) ( ι ( S ) ) > 0 ,
so adjacency in Geo is exactly the edge relation between ι ( R ) and ι ( S ) in N h .
(c)
Attribute recovery. For any numeric attribute A a L loc 1 ( M , μ ) and any R P with 0 < μ ( R ) < ,
1 μ ( R ) R A a d μ Agg a ι ( R ) ,
so the classical region-average is an element of the hypervaluation set.
(d)
Union is a hyperselection. For R , S P there exists a canonical selection map
Sel : R × R R , Sel ( X , Y ) : = X Y ,
such that
Sel ι ( R ) , ι ( S ) ι ( R ) reg ι ( S ) and Sel ι ( R ) , ι ( S ) = R S .
Hence the ordinary union of regions is recovered as a deterministic choice inside the hyperunion.
Consequently, the composite
P ι R Σ
identifies Geo with the singleton slice of HGeo , and HGeo strictly generalizes Geo by allowing operations and evaluations on arbitrary hyperregions X R (finite unions of atoms) rather than only single regions R P .
Proof. 
(a) Injectivity of ι is immediate: if ι ( R ) = ι ( S ) then { R } = { S } , so R = S . Also ι ( R ) = { R } = R .
(b) Using (a) and Definition 10(G1), adjacency R S means H g 1 ( R S ) > 0 . Since ι ( R ) = R and ι ( S ) = S , the stated equivalence follows.
(c) By Definition 11, for X = ι ( R ) we may choose the admissible measurable set E = R ; then
1 μ ( R ) R A a d μ Agg a ι ( R ) .
(d) By definition, Sel ( X , Y ) = X Y X reg Y , so for X = ι ( R ) and Y = ι ( S ) , Sel ( ι ( R ) , ι ( S ) ) = { R , S } ι ( R ) reg ι ( S ) and Sel ( ι ( R ) , ι ( S ) ) = R S . This shows that ordinary union is realized as a distinguished element of the hyperunion, proving that classical region algebra sits inside the hyperalgebra by a canonical choice. □

2.3. (m,n)-SuperHyperGeography

We formalize an (m,n)-SuperHyperGeography, show that its region layer is an ( m , n ) -SuperHyperStructure, and prove that it strictly generalizes the HyperGeography introduced earlier.
Let Geo be as in Definition 10 with measurable region partition P = { R i } i I Σ and let S Σ be a fixed countable family of atomic regions such that
μ M A S A = 0 , 0 < μ ( A ) < , H g 1 ( A ) < ( A S ) ,
and distinct atoms are μ -almost disjoint. To control regularity, we also track the atomic support of a k-level object.
Definition 13
(Atomic support and flattening). Define recursively the atom map At k : P k * ( S ) P * ( S ) and the flattening Υ k : P k * ( S ) Σ by
At 1 ( X ) = X , At k + 1 ( X ) = Y X At k ( Y ) ,
Υ k ( X ) = A At k ( X ) A ( Σ ) .
We say X P k * ( S ) is support-finite if At k ( X ) is finite; write P k , fin * ( S ) for the set of support-finite k-level objects.
Example 10
(Atomic support and flattening at level k = 2 ). Let M R 2 be equipped with the Borel σ-algebra Σ and the Lebesgue area measure μ. Fix three pairwise disjoint measurable atoms S = { A , B , C } Σ with
μ ( A ) = 2 km 2 , μ ( B ) = 3 km 2 , μ ( C ) = 5 km 2 .
Consider the level-2 object
X = { A , B } , { B , C } P 2 * ( S ) = P P 1 * ( S ) { } .
Compute the atomic support and flattening:
1) Atomic support:
At 1 ( { A , B } ) = { A , B } , At 1 ( { B , C } ) = { B , C } ,
At 2 ( X ) = Y X At 1 ( Y ) = { A , B , C } .
Thus X is support-finite and | At 2 ( X ) | = 3 .
2) Flattening:
Υ 2 ( X ) = T At 2 ( X ) T = A B C .
Since A , B , C are pairwise disjoint,
μ Υ 2 ( X ) = μ ( A ) + μ ( B ) + μ ( C ) = 2 + 3 + 5 = 10 km 2 .
This explicitly shows how a level-2 object X induces its atom set At 2 ( X ) and the corresponding ground-set region Υ 2 ( X ) .
Definition 14
(Canonical nesting of atoms). For any nonempty finite T S define the nesting Nest k ( T ) P k , fin * ( S ) by
Nest 1 ( T ) : = T , Nest k + 1 ( T ) : = { Nest k ( T ) } .
Then, by immediate induction,
At k Nest k ( T ) = T , Υ k Nest k ( T ) = A T A .
Example 11
(Canonical nesting of atoms and its identities). Retain the measurable atoms S = { A , B , C } Σ from above, with the same areas, and let
T = { A , C } S ( finite and nonempty ) .
For k = 3 the canonical nesting is
Nest 1 ( T ) = T , Nest 2 ( T ) = { T } , Nest 3 ( T ) = { T } .
We verify the identities in (1):
1) Atomic support:
At 3 Nest 3 ( T ) = Y { { T } } At 2 ( Y ) = At 2 ( { T } ) = Z { T } At 1 ( Z ) = At 1 ( T ) = T = { A , C } .
2) Flattening:
Υ 3 Nest 3 ( T ) = U At 3 ( Nest 3 ( T ) ) U = U { A , C } U = A C .
If A and C are disjoint, then
μ Υ 3 ( Nest 3 ( T ) ) = μ ( A ) + μ ( C ) = 2 + 5 = 7 km 2 .
Hence, concretely, At k ( Nest k ( T ) ) = T and Υ k ( Nest k ( T ) ) = U T U hold for k = 3 , illustrating the general formula.
Definition 15
((m,n)-SuperHyperGeography). Fix integers m , n 1 . The (m,n)-SuperHyperGeography associated with ( M , g , d , μ , Σ ) and atom set S is the tuple
SHGeo ( m , n ) = M , g , d , μ , Σ ; S ; U m , U n ; reg ( m , n ) ; F , α ; A , Agg ( m ) ; N ( m ) , proj ,
where:
(a)
U m : = P m , fin * ( S ) and U n : = P n , fin * ( S ) are the domains/codomains of m- and n-level superobjects.
(b)
The region superhyperoperation (binary, for definiteness)
reg ( m , n ) : U m × U m P U n { }
is defined by
X reg ( m , n ) Y : = Z U n : Υ n ( Z ) = Υ m ( X ) Υ m ( Y ) and At n ( Z ) At m ( X ) At m ( Y ) .
Equivalently, X Y returns all n-level finite packings by atoms from At m ( X ) At m ( Y ) whose geometric union equals Υ m ( X ) Υ m ( Y ) .
(c)
For each geometric feature f = ( S f , dim f , α f ) as in (G2) define the hyperattachment
α f : U m P ( V f ) { } , α f ( X ) : = α f ( x ) : x S f Υ m ( X ) * .
(d)
For a numeric attribute A a L loc 1 ( M , μ ) , define the level-m hypervaluation
Agg a ( m ) ( X ) : = 1 μ ( E ) E A a d μ : E Σ , E Υ m ( X ) , 0 < μ ( E ) < R .
(e)
The level-m hypernetwork N ( m ) = ( G ( m ) , φ ( m ) ) has
V ( m ) = U m , { X , Y } E ( m ) H g 1 Υ m ( X ) Υ m ( Y ) > 0 ,
embedded in M by barycenters/rectifiable arcs along shared boundaries, as in HyperGeography.
Remark 3
(Nonemptiness and locality). For any X , Y U m , the finite set T : = At m ( X ) At m ( Y ) yields
Z 0 : = Nest n ( T ) U n , Υ n ( Z 0 ) = A T A = Υ m ( X ) Υ m ( Y ) ,
so Z 0 X reg ( m , n ) Y ; hence the operation is well-defined and nonempty. All constructions depend only on atoms intersecting Υ m ( X ) Υ m ( Y ) (locality).
Example 12
((2,1)-SuperHyperGeography: multi-agency relief bundles). We instantiate SHGeo ( m , n ) with ( m , n ) = ( 2 , 1 ) to model bundles of service areas proposed by two agencies and their induced single-layer deployment domain.
Ground and atoms.  Let M R 2 be a bounded urban region with Euclidean metric g, Borel σ-algebra Σ, and area measure μ. Fix finite atoms S = { A 1 , A 2 , A 3 , A 4 } Σ with finite-perimeter boundaries and areas (km2)
μ ( A 1 ) = 10 , μ ( A 2 ) = 8 , μ ( A 3 ) = 6 , μ ( A 4 ) = 12 ,
pairwise μ-almost disjoint. Define a population-density field (persons/km2), piecewise constant on atoms:
A pop ( x ) = 8 , 000 x A 1 , 6 , 000 x A 2 , 3 , 000 x A 3 , 2 , 000 x A 4 .
Level-2 superregions (bundles).  Work in U 2 = P 2 , fin * ( S ) . Consider two agencies’ activation bundles
X = { A 1 , A 2 } , { A 3 } , Y = { A 4 } .
By Definition 13, At 2 ( X ) = { A 1 , A 2 , A 3 } , At 2 ( Y ) = { A 4 } and
Υ 2 ( X ) = A 1 A 2 A 3 , Υ 2 ( Y ) = A 4 .
Hence μ Υ 2 ( X ) = 10 + 8 + 6 = 24 and μ Υ 2 ( X ) Υ 2 ( Y ) = 36 (km2).
(2,1)-superhyperoperation.  By (2)–(3), X reg ( 2 , 1 ) Y is the nonempty set of Z U 1 = P 1 , fin * ( S ) such that
Υ 1 ( Z ) = Υ 2 ( X ) Υ 2 ( Y ) = A 1 A 2 A 3 A 4 , At 1 ( Z ) { A 1 , A 2 , A 3 , A 4 } .
A canonical witness is
Z 0 = Nest 1 At 2 ( X ) At 2 ( Y ) = { A 1 , A 2 , A 3 , A 4 } X reg ( 2 , 1 ) Y ,
and by (1) one has Υ 1 ( Z 0 ) = Υ 2 ( X ) Υ 2 ( Y ) .
Concrete calculations (population and demand).  Atomic populations are
Pop ( A 1 ) = 8 , 000 · 10 = 80 , 000 , Pop ( A 2 ) = 6 , 000 · 8 = 48 , 000 ,
Pop ( A 3 ) = 3 , 000 · 6 = 18 , 000 , Pop ( A 4 ) = 2 , 000 · 12 = 24 , 000 .
Thus
Pop Υ 2 ( X ) = 146 , 000 , Pop Υ 2 ( X ) Υ 2 ( Y ) = 170 , 000 .
The average density on the combined deployment domain is
ρ ¯ = Υ 2 ( X ) Υ 2 ( Y ) A pop d μ μ Υ 2 ( X ) Υ 2 ( Y ) = 170 , 000 36 4 , 722.222 persons / km 2 .
If each person requires r = 0.04 relief kits per month, the baseline monthly demand is
D = r · Pop Υ 2 ( X ) Υ 2 ( Y ) = 0.04 × 170 , 000 = 6 , 800 kits .
By (4), the level-2 hypervaluation over X yields the envelope
Agg pop ( 2 ) ( X ) [ 3 , 000 , 8 , 000 ] ,
realized by E A 3 and E A 1 , respectively; for X Y the envelope expands to [ 2 , 000 , 8 , 000 ] . Importantly, any Z X reg ( 2 , 1 ) Y induces the same ground union and hence the same D; only the partitioning differs (e.g., for contracting or governance).
Example 13
((1,2)-SuperHyperGeography: logistics hub governance scenarios). We instantiate SHGeo ( m , n ) with ( m , n ) = ( 1 , 2 ) to represent site alternatives at level 1 and the induced portfolio of governance partitions at level 2.
Ground, atoms, and capacity field.  Let S = { B 1 , B 2 , B 3 } Σ with areas (km2)
μ ( B 1 ) = 5 , μ ( B 2 ) = 7 , μ ( B 3 ) = 4 .
Define a throughput-capacity density (trucks/day/km2),
A cap ( x ) = 120 x B 1 , 80 x B 2 , 150 x B 3 .
Level-1 hyperregions (site selections).  Work in U 1 = P 1 , fin * ( S ) and take
X = { B 1 , B 2 } , Y = { B 3 } .
Then At 1 ( X ) = { B 1 , B 2 } , At 1 ( Y ) = { B 3 } and, by Definition 13,
Υ 1 ( X ) = B 1 B 2 , Υ 1 ( Y ) = B 3 , Υ 1 ( X ) Υ 1 ( Y ) = B 1 B 2 B 3 .
(1,2)-superhyperoperation and admissible outputs.  By (3), X reg ( 1 , 2 ) Y consists of level-2 objects Z U 2 with
Υ 2 ( Z ) = B 1 B 2 B 3 , At 2 ( Z ) { B 1 , B 2 , B 3 } .
Examples (all valid):
Z coarse = Nest 2 { B 1 , B 2 , B 3 } = { B 1 , B 2 , B 3 } , Z split = { B 1 , B 3 } , { B 2 } , Z tri = { B 1 } , { B 2 } , { B 3 } .
By (1), each has Υ 2 ( · ) = B 1 B 2 B 3 while encoding different governance/ownership partitions at level 2.
Concrete calculations (throughput).  Total daily throughput (as an integral of A cap ) over the ground union is
B 1 B 2 B 3 A cap d μ = 120 · 5 + 80 · 7 + 150 · 4 = 600 + 560 + 600 = 1 , 760 trucks / day .
Average capacity density over the union is
κ ¯ = 1 , 760 μ ( B 1 ) + μ ( B 2 ) + μ ( B 3 ) = 1 , 760 16 = 110 trucks / ( day · km 2 ) .
By (4) with m = 1 ,
Agg cap ( 1 ) ( X Y ) = 1 μ ( E ) E A cap d μ : E B 1 B 2 B 3 [ 80 , 150 ] ,
with the endpoints realized on B 2 and B 3 , respectively. Note that κ ¯ and the total 1 , 760 are invariant across all Z X reg ( 1 , 2 ) Y , since they depend only on the flattened ground union; what changes across { Z coarse , Z split , Z tri } is the second-order organization (single operator vs. two-tier vs. fully disaggregated management).
Theorem 3
((m,n)-SuperHyperStructure representation). For fixed m , n 1 , the pair
H reg ( m , n ) : = U m , reg ( m , n )
is an (m,n)-SuperHyperStructure (with arity s = 2 ) on the base set S.
Proof. 
By definition, U m = P m , fin * ( S ) P m ( S ) and the codomain in (2) is a nonempty subset of P n ( S ) . For any X , Y U m , the witness Z 0 = Nest n ( At m ( X ) At m ( Y ) ) U n (see (1)) satisfies the two constraints in (3), so X reg ( m , n ) Y and X reg ( m , n ) Y U n P n ( S ) . Hence reg ( m , n ) is a well-defined ( m , n ) -SuperHyperOperation on S. Therefore U m , reg ( m , n ) is an ( m , n ) -SuperHyperStructure. □
Lemma 2
(Level-1 identification). For all X , Y P 1 , fin * ( S ) one has
X reg ( 1 , 1 ) Y = X reg Y .
Proof. 
When m = n = 1 , At 1 ( · ) is the identity on P 1 , fin * ( S ) and Υ 1 is geometric union of atoms. Thus both definitions coincide verbatim. □
Definition 16
(Canonical embedding into level m). Define ι m : P 1 , fin * ( S ) P m , fin * ( S ) by
ι m ( X ) : = Nest m At 1 ( X ) = Nest m ( X ) .
By (1), Υ m ( ι m ( X ) ) = Υ 1 ( X ) and At m ( ι m ( X ) ) = At 1 ( X ) .
Theorem 4
(SuperHyperGeography generalizes HyperGeography). Let HGeo be the HyperGeography built on S, and let SHGeo ( m , n ) be as in Definition 15. Then:
(a)
Exact recovery at level (1,1). By Lemma 2, SHGeo ( 1 , 1 ) and HGeo have the same region universe and the same hyperoperation.
(b)
Embedding of HyperGeography into level m. The map ι m is injective and satisfies
Υ m ι m ( X ) = Υ 1 ( X ) , At m ι m ( X ) = At 1 ( X ) ,
hence adjacency and attribute evaluations are preserved:
H g 1 Υ 1 ( X ) Υ 1 ( Y ) > 0 H g 1 Υ m ( ι m ( X ) ) Υ m ( ι m ( Y ) ) > 0 ,
1 μ ( R ) R A a d μ Agg a ( m ) ι m ( { R } ) ( choose E = R ) .
(c)
Hyperoperation compatibility. For all X , Y P 1 , fin * ( S ) ,
Nest n At 1 ( X ) At 1 ( Y ) ι m ( X ) reg ( m , n ) ι m ( Y ) ,
and its flattening satisfies
Υ n Nest n ( At 1 ( X ) At 1 ( Y ) ) = Υ 1 ( X ) Υ 1 ( Y ) ,
so the level-m superhyperoperation projects to the same geometric union as in HyperGeography.
Therefore, SHGeo ( m , n ) strictly generalizes HyperGeography by allowing operations/evaluations on m-level superregions with n-level outputs, while recovering the classical case at ( m , n ) = ( 1 , 1 ) .
Proof. 
(a) is Lemma 2. For (b), injectivity of ι m is immediate from Definition 14, and the stated equalities follow from (1). The adjacency equivalence uses those equalities and Definition 10(G1). For the attribute statement, take X = { R } and choose E = R in (4) to obtain the classical region average as an element of Agg a ( m ) ( ι m ( X ) ) .
For (c), using Definition 15 and (1),
At m ( ι m ( X ) ) = At 1 ( X ) , At m ( ι m ( Y ) ) = At 1 ( Y ) ,
thus the candidate Z : = Nest n ( At 1 ( X ) At 1 ( Y ) ) satisfies At n ( Z ) At m ( ι m ( X ) ) At m ( ι m ( Y ) ) and
Υ n ( Z ) = A At 1 ( X ) At 1 ( Y ) A = Υ 1 ( X ) Υ 1 ( Y ) = Υ m ( ι m ( X ) ) Υ m ( ι m ( Y ) ) .
Hence Z ι m ( X ) reg ( m , n ) ι m ( Y ) , proving (5). □

3. Conclusions

In this paper, we examined the viability of employing Hyperstructures and SuperHyperstructures to define HyperGeography and SuperHyperGeography, and we offered a concise discussion that included potential applications. Looking ahead, we hope to see broader set-theoretic extensions of the concepts introduced here, including Fuzzy Sets [42,43], Intuitionistic Fuzzy Sets [44], HyperFuzzy Sets [45,46], Soft Sets [47,48] and HyperSoft Sets [49,50], Rough Sets [51,52] and HyperRough Sets [53], Neutrosophic Sets [54,55], and Plithogenic Sets [56,57]. For example, I would like to explore whether concepts such as Fuzzy Geography (cf.[58,59,60]), Neutrosophic Geography[61,62], and Rough Geography[63,64] can be integrated with the ideas of HyperGeography and SuperHyperGeography, in order to identify new characteristics or potential applications.

Funding

No external funding was received for this work.

Institutional Review Board Statement

This research did not involve human participants or animals, and therefore did not require ethical approval.

Data Availability Statement

This paper is theoretical and did not generate or analyze any empirical data. We welcome future studies that apply and test these concepts in practical settings.

Acknowledgments

We thank all colleagues, reviewers, and readers whose comments and questions have greatly improved this manuscript. We are also grateful to the authors of the works cited herein for providing the theoretical foundations that underpin our study. Finally, we appreciate the institutional and technical support that enabled this research.

Research Integrity

The author confirms that this manuscript is original, has not been published elsewhere, and is not under consideration by any other journal.

Use of Computational Tools

All proofs and derivations were performed manually; no computational software (e.g., Mathematica, SageMath, Coq) was used.

Code Availability

No code or software was developed for this study.

Use of Generative AI and AI-Assisted Tools

We use generative AI and AI-assisted tools for tasks such as English grammar checking, and We do not employ them in any way that violates ethical standards.

Conflicts of Interest

The authors declare no conflicts of interest regarding the publication of this work.

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