Muso

Directory About
Continue with Google
Continue with with Facebook

Top Related Posts

Glacier mass balanceRecessional morainesHanging glaciers as outlet glaciersEvolution of glaciers of SwitzerlandFormer tidewater glaciersReceding glaciersTerminus of mountain glacier turning into a rock glacierTerminus of valley glacier turning into a rock glacierAnimations of glaciersIsostatic rebound

Recent Logins

View Members Directory

Tadhg Kelleher
Last login: 1 day ago
Comments: 0

jacierlogyn
Last login: 3 days ago
Comments: 0

Eileen Lally
Last login: 4 weeks ago
Comments: 0

Özkan Konu
Last login: 1 month ago
Comments: 0

Anne Marie Bevan
Last login: 2 months ago
Comments: 0

Kevin Greene
Last login: 2 months ago
Comments: 0

Retreat of glaciers

Loading Graph...
Press Spacebar to toggle layout
Join the conversation

💬 Know something?

Sign in to leave a note, add a photo, or make a connection.

Continue with Google Continue with Facebook

Keep Muso free

Muso is built by one person, for the love of it. no investors — just your support.

€10
Covers an hour of research
Most popular
€25
Keeps the archive running
€50
Funds a full week of work
✎ Enter my own amount
€5
per month · cancel any time

You'll confirm the amount on the next screen

Donate €25 →
Secure checkout via Stripe  ·  No account needed

Related Images

Paternoster lakes
Dead-ice
Retreat of glaciers in Greenland
Glaciology

Analyzing Network Connections...

Network Profile

Overall Strength
i
91.12% of network
(616)
Strength Breakdown
  • This Post (91.12%)
  • Glacier mass balance (2.37%)
  • Animations of glaciers (0.59%)
  • Bedrock outcrops at glacier termini (0.59%)
  • Evolution of glaciers of Switzerland (0.59%)
  • Former tidewater glaciers (0.59%)
  • Hanging glaciers as outlet glaciers (0.59%)
  • Isostatic rebound (0.59%)
  • Receding glaciers (0.59%)
  • Recessional moraines (0.59%)
  • Terminus of mountain glacier turning into a rock glacier (0.59%)
  • Terminus of valley glacier turning into a rock glacier (0.59%)
  • Glacier mass balance diagrams (0.59%)
Influence Score
i
9.59% of network
(1.27)
Influence Breakdown
  • This Post (9.59%)
  • Glacier mass balance (7.53%)
  • Animations of glaciers (7.53%)
  • Bedrock outcrops at glacier termini (7.53%)
  • Evolution of glaciers of Switzerland (7.53%)
  • Former tidewater glaciers (7.53%)
  • Hanging glaciers as outlet glaciers (7.53%)
  • Isostatic rebound (7.53%)
  • Receding glaciers (7.53%)
  • Recessional moraines (7.53%)
  • Terminus of mountain glacier turning into a rock glacier (7.53%)
  • Terminus of valley glacier turning into a rock glacier (7.53%)
  • Glacier mass balance diagrams (7.53%)
Direct Connections 25

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, 14) = 14
$outbound = max(1, 11) = 11

// 2. Node Base Values (Local connection strength)
Base_Strength (PV) = $inbound * $outbound = 14 * 11 = 154
Base_Influence (IV) = $inbound / $outbound = 14 / 11 = 1.2727

// 3. Exponential Network Values (accumulating 12 direct neighbours)
Network_Strength (CV) = Base_PV * (Neighbour_1_PV * Neighbour_2_PV * ...)
                         = 154 *
                           ( 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 [Recessional moraines] *
                            1 [Terminus of mountain glacier turning into a rock glacier] *
                            1 [Terminus of valley glacier turning into a rock glacier] *
                            1 [Glacier mass balance diagrams]
                           )

                         = 616

Network_Influence (TV) = Base_IV * (Neighbour_1_IV * Neighbour_2_IV * ...)
                         = 1.2727 *
                           ( 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 [Recessional moraines] *
                            1 [Terminus of mountain glacier turning into a rock glacier] *
                            1 [Terminus of valley glacier turning into a rock glacier] *
                            1 [Glacier mass balance diagrams]
                           )

                         = 1.27
Outbound 14 Tags on post
Inbound 11 Posts tagging this
Connections 12 Total nodes
Base Node Strength 154
Base Node Influence 1.2727
Strength Share (vs Direct Neighbours)
91.12% (616 overall)
  • This Post (91.12%)
  • Glacier mass balance (2.37%)
  • Animations of glaciers (0.59%)
  • Bedrock outcrops at glacier termini (0.59%)
  • Evolution of glaciers of Switzerland (0.59%)
  • Former tidewater glaciers (0.59%)
  • Hanging glaciers as outlet glaciers (0.59%)
  • Isostatic rebound (0.59%)
  • Receding glaciers (0.59%)
  • Recessional moraines (0.59%)
  • Terminus of mountain glacier turning into a rock glacier (0.59%)
  • Terminus of valley glacier turning into a rock glacier (0.59%)
  • Glacier mass balance diagrams (0.59%)
Influence Share (vs Direct Neighbours)
9.59% (1.27 overall)
  • This Post (9.59%)
  • Glacier mass balance (7.53%)
  • Animations of glaciers (7.53%)
  • Bedrock outcrops at glacier termini (7.53%)
  • Evolution of glaciers of Switzerland (7.53%)
  • Former tidewater glaciers (7.53%)
  • Hanging glaciers as outlet glaciers (7.53%)
  • Isostatic rebound (7.53%)
  • Receding glaciers (7.53%)
  • Recessional moraines (7.53%)
  • Terminus of mountain glacier turning into a rock glacier (7.53%)
  • Terminus of valley glacier turning into a rock glacier (7.53%)
  • Glacier mass balance diagrams (7.53%)

Connected Network Hierarchy

Sort list by:
Top Network Boosters (Highest Multipliers)
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
Recessional moraines ↗
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
Glacier mass balance diagrams ↗
Str: 1Inf: 1
Weakest Connections (Lowest Multipliers)
Glacier mass balance diagrams ↗
Str: 1Inf: 1
Terminus of valley glacier turning into a rock glacier ↗
Str: 1Inf: 1
Terminus of mountain glacier turning into a rock glacier ↗
Str: 1Inf: 1
Recessional moraines ↗
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

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

Outbound Tags (14)
Animations of glaciers
Bedrock outcrops at glacier termini
Dead-ice
BROKEN LINK
Evolution of glaciers of Switzerland
Former tidewater glaciers
Glacier mass balance
Hanging glaciers as outlet glaciers
Isostatic rebound
Paternoster lakes
BROKEN LINK
Receding glaciers
Recessional moraines
Retreat of glaciers in Greenland
BROKEN LINK
Terminus of mountain glacier turning into a rock glacier
Terminus of valley glacier turning into a rock glacier
Inbound Posts (11)
Glacier mass balance
Animations of glaciers
Bedrock outcrops at glacier termini
Evolution of glaciers of Switzerland
Former tidewater glaciers
Hanging glaciers as outlet glaciers
Isostatic rebound
Receding glaciers
Recessional moraines
Terminus of mountain glacier turning into a rock glacier
Terminus of valley glacier turning into a rock glacier
Last calculated: Jul 2, 12:36 PM
36

Related Content

Topics

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