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Retreat of glaciersGlacier mass balanceEvolution of glaciers of SwitzerlandHanging glaciers as outlet glaciersFormer tidewater glaciersReceding glaciersTerminus of valley glacier turning into a rock glacierAnimations of glaciersTerminus of mountain glacier turning into a rock glacierIsostatic rebound

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Recessional moraines

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Analyzing Network Connections...

Network Profile

Overall Strength
i
0.60% of network
(616)
Strength Breakdown
  • This Post (0.60%)
  • Glacier mass balance (2.38%)
  • Animations of glaciers (0.60%)
  • Bedrock outcrops at glacier termini (0.60%)
  • Evolution of glaciers of Switzerland (0.60%)
  • Former tidewater glaciers (0.60%)
  • Hanging glaciers as outlet glaciers (0.60%)
  • Isostatic rebound (0.60%)
  • Receding glaciers (0.60%)
  • Terminus of mountain glacier turning into a rock glacier (0.60%)
  • Terminus of valley glacier turning into a rock glacier (0.60%)
Dominant nodes (excluded from chart)
Retreat of glaciers 91.67%
Influence Score
i
8.15% of network
(1.27)
Influence Breakdown
  • This Post (8.15%)
  • Retreat of glaciers (10.37%)
  • Glacier mass balance (8.15%)
  • Animations of glaciers (8.15%)
  • Bedrock outcrops at glacier termini (8.15%)
  • Evolution of glaciers of Switzerland (8.15%)
  • Former tidewater glaciers (8.15%)
  • Hanging glaciers as outlet glaciers (8.15%)
  • Isostatic rebound (8.15%)
  • Receding glaciers (8.15%)
  • Terminus of mountain glacier turning into a rock glacier (8.15%)
  • Terminus of valley glacier turning into a rock glacier (8.15%)
Direct Connections 2

Node & Network Details

How is this calculated?

The math continuously tracks how strongly this post is connected to the rest of the network. Every tag forms a 2-way link. The base stats determine personal node strength, and the pie charts below show this node's share against its direct neighbours.

// 1. Base variables (floored at 1 to prevent zero-multiplication math errors)
$inbound = max(1, 1) = 1
$outbound = max(1, 1) = 1

// 2. Node Base Values (Local connection strength)
Base_Strength (PV) = $inbound * $outbound = 1 * 1 = 1
Base_Influence (IV) = $inbound / $outbound = 1 / 1 = 1

// 3. Exponential Network Values (accumulating 11 direct neighbours)
Network_Strength (CV) = Base_PV * (Neighbour_1_PV * Neighbour_2_PV * ...)
                         = 1 *
                           ( 154 [Retreat of glaciers] *
                            4 [Glacier mass balance] *
                            1 [Animations of glaciers] *
                            1 [Bedrock outcrops at glacier termini] *
                            1 [Evolution of glaciers of Switzerland] *
                            1 [Former tidewater glaciers] *
                            1 [Hanging glaciers as outlet glaciers] *
                            1 [Isostatic rebound] *
                            1 [Receding glaciers] *
                            1 [Terminus of mountain glacier turning into a rock glacier] *
                            1 [Terminus of valley glacier turning into a rock glacier]
                           )

                         = 616

Network_Influence (TV) = Base_IV * (Neighbour_1_IV * Neighbour_2_IV * ...)
                         = 1 *
                           ( 1.27 [Retreat of glaciers] *
                            1 [Glacier mass balance] *
                            1 [Animations of glaciers] *
                            1 [Bedrock outcrops at glacier termini] *
                            1 [Evolution of glaciers of Switzerland] *
                            1 [Former tidewater glaciers] *
                            1 [Hanging glaciers as outlet glaciers] *
                            1 [Isostatic rebound] *
                            1 [Receding glaciers] *
                            1 [Terminus of mountain glacier turning into a rock glacier] *
                            1 [Terminus of valley glacier turning into a rock glacier]
                           )

                         = 1.27
Outbound 1 Tags on post
Inbound 1 Posts tagging this
Connections 11 Total nodes
Base Node Strength 1
Base Node Influence 1
Strength Share (vs Direct Neighbours)
0.60% (616 overall)
  • This Post (0.60%)
  • Glacier mass balance (2.38%)
  • Animations of glaciers (0.60%)
  • Bedrock outcrops at glacier termini (0.60%)
  • Evolution of glaciers of Switzerland (0.60%)
  • Former tidewater glaciers (0.60%)
  • Hanging glaciers as outlet glaciers (0.60%)
  • Isostatic rebound (0.60%)
  • Receding glaciers (0.60%)
  • Terminus of mountain glacier turning into a rock glacier (0.60%)
  • Terminus of valley glacier turning into a rock glacier (0.60%)
Dominant nodes (excluded from chart)
Retreat of glaciers 91.67%
Influence Share (vs Direct Neighbours)
8.15% (1.27 overall)
  • This Post (8.15%)
  • Retreat of glaciers (10.37%)
  • Glacier mass balance (8.15%)
  • Animations of glaciers (8.15%)
  • Bedrock outcrops at glacier termini (8.15%)
  • Evolution of glaciers of Switzerland (8.15%)
  • Former tidewater glaciers (8.15%)
  • Hanging glaciers as outlet glaciers (8.15%)
  • Isostatic rebound (8.15%)
  • Receding glaciers (8.15%)
  • Terminus of mountain glacier turning into a rock glacier (8.15%)
  • Terminus of valley glacier turning into a rock glacier (8.15%)

Connected Network Hierarchy

Sort list by:
Top Network Boosters (Highest Multipliers)
Retreat of glaciers ↗
Str: 154Inf: 1.27
Glacier mass balance ↗
Str: 4Inf: 1
Animations of glaciers ↗
Str: 1Inf: 1
Bedrock outcrops at glacier termini ↗
Str: 1Inf: 1
Evolution of glaciers of Switzerland ↗
Str: 1Inf: 1
Former tidewater glaciers ↗
Str: 1Inf: 1
Hanging glaciers as outlet glaciers ↗
Str: 1Inf: 1
Isostatic rebound ↗
Str: 1Inf: 1
Receding glaciers ↗
Str: 1Inf: 1
Terminus of mountain glacier turning into a rock glacier ↗
Str: 1Inf: 1
Terminus of valley glacier turning into a rock glacier ↗
Str: 1Inf: 1
Weakest Connections (Lowest Multipliers)
Terminus of valley glacier turning into a rock glacier ↗
Str: 1Inf: 1
Terminus of mountain glacier turning into a rock glacier ↗
Str: 1Inf: 1
Receding glaciers ↗
Str: 1Inf: 1
Isostatic rebound ↗
Str: 1Inf: 1
Hanging glaciers as outlet glaciers ↗
Str: 1Inf: 1
Former tidewater glaciers ↗
Str: 1Inf: 1
Evolution of glaciers of Switzerland ↗
Str: 1Inf: 1
Bedrock outcrops at glacier termini ↗
Str: 1Inf: 1
Animations of glaciers ↗
Str: 1Inf: 1
Glacier mass balance ↗
Str: 4Inf: 1
Retreat of glaciers ↗
Str: 154Inf: 1.27

Connection Health Audit (Red = broken 1-way link)

Outbound Tags (1)
Retreat of glaciers
Inbound Posts (1)
Retreat of glaciers
Last calculated: Jun 15, 7:19 AM
26

Related Content

Topics

  • Hanging glaciers as outlet glaciers
  • Isostatic rebound
  • Retreat of glaciers
  • Receding glaciers
  • Glacier mass balance
  • Terminus of mountain glacier turning into a rock glacier
  • Animations of glaciers
  • Terminus of valley glacier turning into a rock glacier
  • Bedrock outcrops at glacier termini
  • Evolution of glaciers of Switzerland
  • Former tidewater glaciers