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The factors controlling the development of these two landforms are still poorly understood.
In this regard, restoration plantings in the Lurg Hills generally developed in different ways across the two landforms studied (i.e., upper and lower hills).
Five age classes (unrestored, 4 6 years old, 8 10 years old, 12 14 years old and remnant areas) and two landforms (upper hills and lower hills) were considered.
A total of 42 sites were sampled equally across the two landforms (Table 1), each of which contained 15 restored sites (comprising 5 in each of three age categories), five unrestored sites and one remnant site, with the restored sites being randomly selected to ensure site selection was objective and unbiased.
In August 1933, a hurricane created an inlet south of Ocean City, Maryland, separating the two landforms.
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The original regeneration treatments followed a split-split plot experimental design on two landform types (LF), four ground scarification treatments (GST) plus a non-scarified control, and five artificial white spruce regeneration treatments (WSRT) plus a natural seedfall control (Densmore et al., 1999).
The semiactive CEA class occurred predominantly on all three landforms.
For both 1985 and 1999, the four landforms exhibited increasing degrees of degradation in the following order: low mountains > lava tablelands > hills > high plains.
At these six landforms, we studied ground thermal conditions, freeze-thaw cycles, and snow dynamics using a combination of in situ monitoring and C-band radar satellite data in the period 2005 2012.
Also, the aggregation of geomorphons to five landforms to predict soil property distribution on the landscape gave promising results for the low-relief and relatively flat area of northeast Indiana.
Eight landform types have been defined by their geomorphological form, geometry, grain size parameters, stratification, fabric and rock contacts.
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