Name: OLD AQUEDUCT ON THE CONEMAUGH. John Augustus Hows, 1832 - 1874. The Conemaugh River is formed at Johnstown in southwestern Cambria County by the confluence of the Little Conemaugh and Stonycreek rivers. It flows generally WNW, in a winding course through the mountains along the northern edge of Laurel Hill and Chestnut Ridge. Northwest of Blairsville it is joined by Blacklick Creek. At Saltsburg it is joined from the south by Loyalhanna Creek to form the Kiskiminetas River. USA - SuperStock
Brand: Artokoloro
SKU: 4443-20927
Availability: InStock

OLD AQUEDUCT ON THE CONEMAUGH. John Augustus Hows, 1832 - 1874. The Conemaugh River is formed at Johnstown in southwestern Cambria County by the confluence of the Little Conemaugh and Stonycreek rivers. It flows generally WNW, in a winding course through the mountains along the northern edge of Laurel Hill and Chestnut Ridge. Northwest of Blairsville it is joined by Blacklick Creek. At Saltsburg it is joined from the south by Loyalhanna Creek to form the Kiskiminetas River. USA

SuperStock offers millions of photos, videos, and stock assets to creatives around the world. This image of OLD AQUEDUCT ON THE CONEMAUGH. John Augustus Hows, 1832 - 1874. The Conemaugh River is formed at Johnstown in southwestern Cambria County by the confluence of the Little Conemaugh and Stonycreek rivers. It flows generally WNW, in a winding course through the mountains along the northern edge of Laurel Hill and Chestnut Ridge. Northwest of Blairsville it is joined by Blacklick Creek. At Saltsburg it is joined from the south by Loyalhanna Creek to form the Kiskiminetas River. USA by Artokoloro is available for licensing today.