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{| class = "wikitable"
 
{| class = "wikitable"
 
|-
 
|-
! Type
+
! Type || Description
! Description
   
|-
 
|-
| I
+
| I || Rocks with pores capable of producing gas without natural or artificial fracturing.
| Rocks with pores capable of producing gas without natural or artificial fracturing.
   
|-
 
|-
| II
+
| II || Rocks with pores capable of producing gas with natural or artificial fracturing and/or interbedded with type I rocks.
| Rocks with pores capable of producing gas with natural or artificial fracturing and/or interbedded with type I rocks.
   
|-
 
|-
| III
+
| III || Rocks too tight to produce at commercial rates even with natural or artificial fracturing.
| Rocks too tight to produce at commercial rates even with natural or artificial fracturing.
   
|}
 
|}
   Line 50: Line 46:  
{| class = "wikitable"
 
{| class = "wikitable"
 
|-
 
|-
! rowspan ="2" | Pore type
+
! rowspan ="2" | Pore type || colspan="3" | Characteristics of dry, freshly broken surfaces at 20× magnification || rowspan ="2" | Permeability
! colspan="3" | Characteristics of dry, freshly broken surfaces at 20× magnification
  −
! rowspan ="2" | Permeability
   
|-
 
|-
! Visible
+
! Visible || Pinpoint || Consolidation
! Pinpoint
  −
! Consolidation
   
|-
 
|-
| I
+
| I || Abundant to common; interconnection visible on many pores || Very abundant to common || Needle probe easily dislodges many grains from rock surface || ''Type I Subclasses''<br>IA:>100md<br>IB: 10–100 md<br>IC: 1–10 md<br>ID: ±0.5–1 md
| Abundant to common; interconnection visible on many pores
  −
| Very abundant to common
  −
| Needle probe easily dislodges many grains from rock surface
  −
| ''Type I Subclasses''<br>IA:>100md<br>IB: 10–100 md<br>IC: 1–10 md<br>ID: ±0.5–1 md
   
|-
 
|-
| II
+
| II || Scattered || Abundant to common || Needle probe can only occasionally dislodge a grain from rock surface || ± 0.5–1.0 md (depending on particle size, sorting, and clay mineral content)
| Scattered
  −
| Abundant to common
  −
| Needle probe can only occasionally dislodge a grain from rock surface
  −
| ± 0.5–1.0 md (depending on particle size, sorting, and clay mineral content)
   
|-
 
|-
| style=white-space:nowrap | III
+
| style=white-space:nowrap | III || None to very isolated || None to a few pores || Usually very well consolidated and/or pores filled with clays or other pore-filling material || Too tight to produce gas at commercial rates even when fractured or interbedded with type I rocks
| None to very isolated
  −
| None to a few pores
  −
| Usually very well consolidated and/or pores filled with clays or other pore-filling material
  −
| Too tight to produce gas at commercial rates even when fractured or interbedded with type I rocks
   
|}
 
|}
  

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