1 / 33

SHORELINE EROSION AT MAD ISLAND MARSH PRESERVE.

SHORELINE EROSION AT MAD ISLAND MARSH PRESERVE. Mad Island Marsh Preserve is a 3,148-acre tract containing the east arm of Mad Island Lake, its associated freshwater and brackish marshes, and surrounding upland prairie and shrub-land habitats. Dredge spoils. Spartina marsh.

tashya-stokes
Download Presentation

SHORELINE EROSION AT MAD ISLAND MARSH PRESERVE.

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. SHORELINE EROSION AT MAD ISLAND MARSH PRESERVE. Mad Island Marsh Preserve is a 3,148-acre tract containing the east arm of Mad Island Lake, its associated freshwater and brackish marshes, and surrounding upland prairie and shrub-land habitats. Dredge spoils Spartina marsh Gulf Intracoastal Water Way Harry Williams, Geomorphology

  2. Harry Williams, Geomorphology

  3. The Gulf Intracoastal Water Way, constructed in 1941, cuts through the southern portion of the Preserve and is flanked to the south by man-made islands of dredge spoils. Dredgespoils GIWW - view west. Preserve Harry Williams, Geomorphology

  4. Considerable wave erosion has occurred, and continues to occur, along the Preserve shorelines bordering the Waterway. Shorelines along the Waterway are eroded by waves generated by barge traffic. Harry Williams, Geomorphology

  5. 1992 1993 Eroded road. Harry Williams, Geomorphology

  6. This fence was constructed several feet back from the shore one year before this photo was taken. Undercutting has caused this block of soil to fall into the GIWW. It has also destroyed the boat ramp. Harry Williams, Geomorphology

  7. The erosion is caused by waves cutting a wave-cut notch and causing collapse and cliff formation. Harry Williams, Geomorphology

  8. A large Spartina marsh borders the GIWW along part of the preserve shoreline. This is a valuable wildlife habitat. It is also being eroded by wave action. Harry Williams, Geomorphology

  9. There is a sharp cliff here too (hidden by high tide in this photo). Harry Williams, Geomorphology

  10. notch The resulting cliff edge is easily identified on air photos. Harry Williams, Geomorphology

  11. The research study was conducted in order to provide information on the location and rate of shoreline erosion along the shores of the preserve over the last fifty years. Long-term rates of shoreline erosion were established by the analysis of sequential aerial photographs taken in 1930, 1943, 1958, 1978 and 1991. The shoreline from each photograph was transferred onto a single base map. Movement of the shoreline at selected points was measured and converted to feet (or meters) of erosion per year. 80 feet 80 feet in 20 years = 4 feet per year. 1978shoreline 1958shoreline Harry Williams, Geomorphology

  12. 1930 Harry Williams, Geomorphology

  13. 1943 Harry Williams, Geomorphology

  14. 1958 Harry Williams, Geomorphology

  15. 1978 Harry Williams, Geomorphology

  16. 1991 Harry Williams, Geomorphology

  17. Base map. Harry Williams, Geomorphology

  18. Measurement locations: A…Z = shoreline migration; 1..4 width of GIWW. The main preserve shoreline = A - I. Harry Williams, Geomorphology

  19. MAD ISLAND PRESERVE, SHORELINE MIGRATION: 1943-1991 SITE 1943‑1958 1958‑1978 1978‑1991 1943‑1991 FEET FT/YR FEET FT/YR FEET FT/YR FEET FT/YR A 84 5.6 53 2.7 49 3.7 186 3.9 B 88 5.9 44 2.2 53 4.1 186 3.9 C 27 1.8 62 3.1 53 4.1 142 2.9 D 35 2.4 41 2.0 18 1.4 94 2.0 E 0 0.0 88 4.4 80 6.1 168 3.5 F 0 0.0 53 2.7 62 4.8 115 2.4 G 0 0.0 35 1.8 71 5.4 106 2.2 H 0 0.0 31 1.5 71 5.4 102 2.1 I 0 0.0 44 2.2 27 2.0 71 1.5 J 0 0.0 35 1.8 0 0.0 35 0.7 For the main preserve shoreline, erosion rates for the most recent period (1978-1991) vary from 0 to 6.1 feet per year. WIDTH OF WATERWAY (feet) RATIO: SITE 1943 1958 1978 1991 1991/1943 1 150 230 425 469 313% 2 212 336 504 531 250% 3 212 292 513 593 280% 4 195 354 531 558 286% The width of the water way increased by an average of 282%. Harry Williams, Geomorphology

  20. An important finding of the study is that severe erosion is occurring near the entrance to Mad Island Bayou. Bayou entrance Harry Williams, Geomorphology

  21. 1943 1991 Harry Williams, Geomorphology

  22. 1992 1993 1994 Views west from the end of the peninsula. Harry Williams, Geomorphology

  23. GIWW Bayou The large bend in the bayou was about 24 feet from the GIWW in 1994. Breaching of the peninsula at this point would abruptly shorten Mad Island Bayou by several hundred meters and probably increase salt water intrusion into Mad Island Lake. Harry Williams, Geomorphology

  24. Partly as a result of this study, the Nature Conservancy of Texas built concrete erosion barriers along this part of the preserve shoreline in 1996 - so far they appear to be working - there has been no more erosion along this part of the shoreline. Harry Williams, Geomorphology

  25. UPDATE: In 2005, a grad student (Webster Mangham) did a Masters thesis on erosion at MIMP between 1995 and 2005. He used GPS, DOQQs and GIS. Harry Williams, Geomorphology

  26. The concrete mat still looks pretty good (in places) after 9 years. Harry Williams, Geomorphology

  27. BUT – in other places it has clearly failed – the soil has been washed out from under it and it has collapsed. Harry Williams, Geomorphology

  28. Harry Williams, Geomorphology

  29. Harry Williams, Geomorphology

  30. Harry Williams, Geomorphology

  31. Harry Williams, Geomorphology

  32. 1991 Harry Williams, Geomorphology

  33. Harry Williams, Geomorphology

More Related