By Ranger Steve Mueller
Water flows from high to low areas and over time it shortens its path. Tadpole Pond, at Howard Christensen Nature Center (HCNC), is higher than Chrishaven Lake, Spring Lake, Spring Creek, and Rogue River. The route water takes from Tadpole Pond to the Rogue River has a “youthful” geology.
Surrounding Tadpole Pond, rain and snowmelt drains a small area of higher ground to feed the pond. The pond was dredged deeper before becoming HCNC. The dredging cut deeper below the water table and allowed water to enter the pond from surrounding groundwater. This created a permanent shallow pond. An earth dam was constructed at the east end of the pond, with an overflow drain installed under Nature’s Habitats Trail leading toward Chrishaven Lake.
From the pond, water flows east into a boggy swamp that fills a glacial kettle lake basin formed 8000 years ago. A large block of ice left by a retreating glacier was buried and slowly melted. The melt water filled the resulting lake depression. Chrishaven Lake has been shrinking in size as vegetation gradually fills from shorelines.
Chrishaven Lake Boardwalk begins at the edge of an ancient 8000 year old shoreline and makes its way to the current open water of the lake. We cannot see open water from the ancient shoreline where the boardwalk begins. Water from Tadpole Pond makes its way through the swamp, enters the lake, and exits eastward through what was once part of the open water lake. Water continues flowing eastward saturating swampland forest where open water was once present. A small stream channel flows from the lake and crosses Nature’s Habitats Trail where a boardwalk leads through the lowland near the Swamp Shelter building.
View of the creek is lost as it merges into a large wetland forest on it way to Spring Lake. At one time Chrishaven Lake and Spring Lake may have been connected with open water. When water reaches Spring Lake, it no longer continues eastward. Spring Creek coming from north of 20 Mile Road enters Spring Lake and flows out its southwest corner. Upstream from the lake, Spring Creek is small. Where it exits the lake, the stream is about 30 feet wide because additional water feeds the creek from springs in the lake.
The east flowing water from Tadpole Pond turns westward and flows south of Chrishaven Lake and Tadpole Pond on its way west to the Rogue River. Given time, the water will flow directly west to the Rogue River from Tadpole Pond. Water takes the least resistant route. The current landscape is geologically known as youthful because water flow does not all converge directly toward Rogue River but follows an erratic path.
Given time, water will carry land away particle by particle to create a channel directly from Tadpole Pond to Rogue River. We will not live thousands of years to witness landscape changes that develop a mature river system and then an old geologic river system. Details of change from geologic youth to mature, and old age river systems will need to wait for another time.
During our lives, enjoy varied nature niches at HCNC that have developed along a youthful water course that flows east from Tadpole Pond to Spring Lake and turns 180 degrees to flow west to Rogue River. Dramatically different nature niches enhance biodiversity along the meandering watercourse. Visit HCNC and purchase an individual or family membership at the Red Pine Interpretive Center. HCNC has perhaps wildest and most diverse habitat variety of any designated nature study areas in Kent County.
Natural history questions or topic suggestions can be directed to Ranger Steve (Mueller) at email@example.com Ody Brook, 13010 Northland Dr, Cedar Springs, MI 49319-8433. 616-696-1753.