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Soil Survey of Crater Lake National Park, Oregon 

General Soil Map Units

 

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Soils That Are in Valleys and Formed in Ash and Pumice Flow Deposits of Ash, Pumice, and Cinders

 

Number of map units: 4

Percentage of park: 42 percent

 

4. Maklak-Collier (ponderosa pine/fir with lodgepole pine)

 

Percentage of park: 5 percent

Location in park: Lowlands and valleys, mainly near the eastern and southeastern boundaries

Depth class: Very deep

Position on landscape: Pumice flows and ashflows

Parent material: Pumice, ash, and cinders

Elevation: 4,000 to 6,000 feet

Average annual precipitation: 20 to 60 inches

Average annual air temperature: 38 to 44 degrees F

Frost-free period: 0 to 50 days

Minor components: 5 percent Lapine soils

Present vegetation: Ponderosa pine, white fir, and lodgepole pine

 

Maklak soils

 

Drainage class: Excessively drained

Permeability: Very rapid

Surface texture: Paragravelly ashy loamy sand

Subsoil texture: Very paragravelly ashy loamy sand

Substratum texture: Extremely paragravelly ashy loamy sand

Slope range: 0 to 10 percent

 

Collier soils

 

Drainage class: Somewhat excessively drained

Permeability: Rapid

Surface texture: Ashy sandy loam

Subsoil texture: Paragravelly ashy loamy sand

Substratum texture: Paragravelly ashy sand

Slope range: 0 to 80 percent

 

 

 

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