In the wake of collapse, the fate of these groups living along the southeastern periphery seemed to vary between areas.
The response of fishes to periodic spring floods in a southeastern stream.
Progressive non-coaxial deformation continued in the southeastern antiform and is recorded by late-synkinematic growth of cordierite.
The results reveal clockwise rotations in the northeast and anticlockwise rotations in the west and southeastern corner of the basin.
Metasedimentary samples from the southeastern portion are represented by graphite schist and metapelite.
No distinction between samples from the northwestern and southeastern parts of the section is discernible.
Keynes children, as a group, are taking par t in this general southeastern change.
Since that time, the parasite has adapted to this snail species which is now an efficient host along the southeastern coastal region of the country.
