Major Land Resource Area 096X
Northwestern Michigan Fruit Belt
Accessed: 11/21/2024
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Ecological site list
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i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon.
- Loamy Site: < 80% sand in the top 150 cm or < 70% sand in the top 50 cm; and not in ultic subgroup unless pH ≥6 or clay ≥20%.
- No seasonal water table (well drained or drier).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon.
- Loamy Site: < 80% sand in the top 150 cm or < 70% sand in the top 50 cm; and not in ultic subgroup unless pH ≥6 or clay ≥20%.
- Seasonal water table present within 100 cm of surface (moderately well drained or wetter).
- Non-hydric Soil (somewhat poorly to moderately well drained).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon.
- Loamy Site: < 80% sand in the top 150 cm or < 70% sand in the top 50 cm; and not in ultic subgroup unless pH ≥6 or clay ≥20%.
- Seasonal water table present within 100 cm of surface (moderately well drained or wetter).
- Hydric Soil (poorly or very poorly drained).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon.
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- No water table within 100 cm of surface (well drained or drier).
- Signs of higher productivity and infrequent fire: Bhs horizon present (dark reddish brown layer of organic matter and iron-aluminum oxides).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon.
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- No water table within 100 cm of surface (well drained or drier).
- Signs of lower productivity and frequent fire: Bhs horizon absent (lacking a dark reddish brown layer of organic matter and iron-aluminum oxides).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon.
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- Seasonal water table present within 100 cm of surface (moderately well drained or wetter).
- Non-hydric Soil (somewhat poorly to moderately well drained).
- pH < 5.5 in the top 50 cm, Spodosols, or Spodic and Ultic subgroups.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon.
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- Seasonal water table present within 100 cm of surface (moderately well drained or wetter).
- Hydric Soil (poorly or very poorly drained).
- pH < 5.5 in the top 50 cm, Spodosols, or Spodic and Ultic subgroups.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon.
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- Seasonal water table present within 100 cm of surface (moderately well drained or wetter).
- Non-hydric Soil (somewhat poorly to moderately well drained).
- pH ≥ 5.5 in the top 50 cm, Mollisols, or Mollic subgroups.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon.
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- Seasonal water table present within 100 cm of surface (moderately well drained or wetter).
- Hydric Soil (poorly or very poorly drained).
- pH ≥ 5.5 in the top 50 cm, Mollisols, or Mollic subgroups.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Floodplain.
- Non-hydric Soil (somewhat poorly to well drained).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Floodplain.
- Hydric Soil (poorly or very poorly drained).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Histosol or Histic Subgroup.
- Mean pH of the top 50 cm ≥ 5.0, or euic reaction class.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- North of the Manistee River, cooler summer, more winter snow.
- Non-Floodplain.
- Histosol or Histic Subgroup.
- Mean pH of the top 50 cm < 5.0, or dysic reaction class.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon (if any peat or muck surface, it is < 20 cm thick).
- Loamy Site: < 80% sand in the top 150 cm or < 70% sand in the top 50 cm; and not in ultic subgroup unless pH ≥6 or clay ≥20%.
- No water table (well drained or drier).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon (if any peat or muck surface, it is < 20 cm thick).
- Loamy Site: < 80% sand in the top 150 cm or < 70% sand in the top 50 cm; and not in ultic subgroup unless pH ≥6 or clay ≥20%.
- Seasonal water table present (moderately well drained or wetter).
- Non-hydric Soil (somewhat poorly to moderately well drained).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon (if any peat or muck surface, it is < 20 cm thick).
- Loamy Site: < 80% sand in the top 150 cm or < 70% sand in the top 50 cm; and not in ultic subgroup unless pH ≥6 or clay ≥20%.
- Seasonal water table present (moderately well drained or wetter).
- Hydric Soil (poorly or very poorly drained).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon (if any peat or muck surface, it is < 20 cm thick).
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- No water table within 100 cm of surface (well drained or drier).
- Signs of higher productivity and infrequent fire: Spodic subgroup or Spodosol (reddish or reddish brown layer of organic matter and iron-aluminum oxides), or pH of top 50 cm ≥ 6, or depth to carbonates < 100 cm deep.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon (if any peat or muck surface, it is < 20 cm thick).
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- No water table within 100 cm of surface (well drained or drier).
- Signs of lower productivity and frequent fire: Not Spodic subgroup nor Spodosol (reddish or reddish brown layer of organic matter and iron-aluminum oxides), and pH of top 50 cm < 6, and depth to carbonates ≥ 100 cm.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon (if any peat or muck surface, it is < 20 cm thick).
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- Seasonal water table present within 100 cm of surface (moderately well drained or wetter)
- Non-hydric Soil (somewhat poorly to moderately well drained).
- pH < 5.5 in the top 50 cm, Spodosols, or Spodic and Ultic subgroups.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon (if any peat or muck surface, it is < 20 cm thick).
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- Seasonal water table present within 100 cm of surface (moderately well drained or wetter)
- Hydric Soil (poorly or very poorly drained).
- pH < 5.5 in the top 50 cm, Spodosols, or Spodic and Ultic subgroups.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon (if any peat or muck surface, it is < 20 cm thick).
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- Seasonal water table present within 100 cm of surface (moderately well drained or wetter)
- Non-hydric Soil (somewhat poorly to moderately well drained).
- pH ≥ 5.5 in the top 50 cm, Mollisols, or Mollic subgroups.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Mineral Soil with no histic epipedon (if any peat or muck surface, it is < 20 cm thick).
- Sandy Site: ≥ 80% sand in the top 150 cm and ≥ 70% sand in the top 50 cm; or ≥ 80% sand in top 50 cm; or < 20% clay in top 150 cm, pH <6, and ultic subgroup.
- Seasonal water table present within 100 cm of surface (moderately well drained or wetter)
- Hydric Soil (poorly or very poorly drained).
- pH ≥ 5.5 in the top 50 cm, Mollisols, or Mollic subgroups.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Floodplain.
- Non-hydric Soil (somewhat poorly to well drained).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Floodplain.
- Hydric Soil (poorly or very poorly drained).
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Histosol or Histic Subgroup (peat or muck surface ≥ 20 cm thick).
- Mean pH of the top 50 cm ≥ 5.0, or euic reaction class.
-
i
Key Characteristics
- Inland.
- Deep Soil or Water Table.
- South of Manistee River, warmer summer, less winter snow.
- Non-Floodplain.
- Histosol or Histic Subgroup (peat or muck surface ≥ 20 cm thick).
- Mean pH of the top 50 cm < 5.0, or dysic reaction class.
-
i
Key Characteristics
- Sites immediately adjacent to the Great Lakes, river mouths and shoreline, affected by water levels of the Great Lakes.
- Storm washed beach and active windblown dunes
-
i
Key Characteristics
- Sites immediately adjacent to the Great Lakes, river mouths and shoreline, affected by water levels of the Great Lakes.
- River mouths.
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