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If this is done, the evidence clearly indicates that the magnetic poles have slowly wandered across the globe with respect to sections of the crust on which datable rock samples are found.
All the samples are found to be polycrystalline in nature.
The shale samples are found to be clay rich.
All the rock samples are found to be surface fractals.
Except the bulk MmNi5 alloy, other samples are found to absorb hydrogen in the first cycle.
More than 70%% of groundwater samples are found with fluoride concentration exceeding from 1.0 mg/L.
The samples are found to exhibit large optical nonlinearity, leading to optical limiting behavior.
Comparisons among diffraction spectra and hierarchical cluster analysis of these spectra for all samples are found in Figure 5.
Therefore, the majority of groundwater samples are found to be safe for drinking and irrigation management practices.
The total hardness indicates that majority of the groundwater samples are found within the permissible limit of WHO.
Based on the total hardness and TDS, 96%% of groundwater samples are found suitable for drinking purpose.
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