Each May, since 2002, Cleveland Heights has celebrated National Preservation Month. Since 2013, the activities have featured a walking tour series called Cleveland Heights Rocks and Waters. The tours pose questions about the places in which we live. How does a neighborhood landscape come to be? What does nature provide? Can humans live in ways to honor the gift?
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Rocks and Waters walking tours
1. Rocks and Waters: Cleveland Heights deep history
by Roy Larick, Bluestone Heights
Each May, since 2002, Cleveland Heights has celebrated
National Preservation Month. Since 2013, the annual
activities have featured a walking tour series called Cleveland
Heights Rocks and Waters.
The tours pose questions about the places in which we live.
How does a neighborhood landscape come to be? What does
nature provide? Can humans live in ways to honor the gift?
Rocks and Waters finds answers along neighborhood stream
courses. At such places, natural and human forces combine to
shape landscapes. The resulting mixture always makes for an
intriguing visit. On such visits, we gain insights on local life
issues and on the good and bad of place planning. We see
what once was, what we now have, and how it could be better.
Deep History Rocks and Waters looks for the elemental
forces giving rise to natural landforms. We also seek the
weave of natural and human actions that make current places
special—and sometimes startling. Stated simply, the walks
explore the deep history of small-scale Heights landscapes.
On the East Side, the Portage Escarpment is the primary
natural feature. It forms the local transition between North
America’s Central Lowland and Appalachian Highland.
Cleveland Heights sits squarely on the escarpment. We can
comprehend the place from two perspectives of nature: how
the landforms arose and how current streams take them down.
Landforms The old forces that shaped Portage Escarpment
landforms included bedrock deposition, tectonic uplift and
glaciation. Local bedrock includes two hard sandstone beds:
the Euclid bluestone and the Berea Sandstone. Glacial action
carved out two narrow terraces upon these beds: the bluestone
terrace and, just above, the sandstone terrace. As the Euclid
bluestone is found only on the East Side, the bluestone terrace
is a uniquely Heights landform.
Streams Within the city, three creeks cut through the terraces
on their ways to Lake Erie: Doan Brook, the Dugway Brooks
(west and east branches) and Nine Mile Creek. The stream
ravines evince the power of water to tear down. As such, the
ravines are windows into the old bedrock-making forces.
The streams have small headwater tributaries in Cleveland
Heights, three of which are the basis for walking tours: Blue
Rock Brook (Doan), Compton Run (Dugway east) and
Quilliams Creek (Nine Mile). Two other walks cover trunk
stream segments of Dugway’s east and west branches.
Portage Escarpment with select Heights suburbs.
May 2013: Barrow & Larick begin the Blue Rock Brook walk.
Portage Escarpment with Rocks and Waters stream areas.
Portage Escarpment bedrock and stream profile.
Dave Lawrence