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The Daily Dispatch: March 1, 1865., [Electronic resource], article 1 (search)
The following is the official account of the occupation of Wilmington by the Federal forces: Fortress Monroe, Virginia, February 24--10 P. M. To General U. S. Grant, City Point: Our troops entered Wilmington on the morning of the 22d instant. After the evacuation of Fort Anderson, General Schofield directed Coed to march at a moment's notice; and considerable commotion within the rebel lines was displayed yesterday.--There are also rumors that Lee meditates an attack on Grant. All these matters, taken in connection with the fact that the rebel journals have received orders from the authorities to be particularly reticent regarding milie result. The Tribune finally settles us by this summing up: Thus, day after day, and with capture after capture, the great game goes on to its culmination. Grant watching and waiting at Petersburg, Sherman driving on through South and North Carolina with irresistible force, Schofield advancing from Wilmington, and Sheridan
The Daily Dispatch: March 1, 1865., [Electronic resource], article 1 (search)
The News. The Richmond and Petersburg lines. Nothing of importance has occurred on these lines. There was some shelling at Petersburg on Monday, but, as usual, it affected nothing. Grant still has his forces massed on Hatcher's run, waiting for dry weather and firm roads. There is a report that, weather favoring, he will, when he next strikes his tents, attempt an extensive flank movement around our right. The Valley. The enemy, on yesterday, were approaching Staunton in heavy force from the Valley — chiefly cavalry. From the South. We are still without official intelligence of movements now taking place in the Carolinas, and, for reasons hitherto stated, do not care to repeat all the reports that reach us. We heard yesterday that Sherman was stuck in the mud in one of the Southern States. If it has rained half as much there as in this vicinity, there can be no doubt of the truth of the statement. There have been many widely-different estimates of th