CONTENTS
PURPOSE AND SCOPE OF THE GUIDE HOW TO USE THE GEOLOGY AND NATURAL ENVIRONMENTS MAP MAP CONSTRUCTION ORIGIN AND GEOLOGIC HISTORY OF PADRE ISLAND HISTORY OF ISLAND DEVELOPMENT THE DYNAMIC GULF SHORELINE ENVIRONMENTS OF PADRE ISLAND AND LAGUNA MADRE BARRIER SYSTEM HISTORY OF HUMAN ACTIVITY ON PADRE ISLAND KARANKAWA INDIANS FIELD TRIP THROUGH THE ENVIRONMENTS OF NORTH PADRE ISLAND INDEX (omitted from the online edition) FIGURES 1. Index and location maps for Padre Island and the surrounding area 2. Generalized cross section of north Padre Island environments, from the Gulf shoreline to Laguna Madre 3. Annual average precipitation along Texas coast and monthly precipitation data for Corpus Christi and Port Isabel, Texas 4. Annual average temperatures along Texas coast and average monthly temperatures for Corpus Christi and Brownsville, Texas 5. Annual frequency of surface wind directions as determined over the period 1951 to 1960 6. Index map of the northern part of Padre Island National Seashore 7. Observation deck and walkway at Malaquite Beach visitor facilities 8. Paved campground just north of Malaquite Beach visitor facilities 9. Four-wheel-drive warning sign 10. Beach marker showing the approximate mileage from the south beach access road near Malaquite Beach 11. Intracoastal Waterway, approximately 12 feet deep, paralleled by a row of spoil heaps 12. Petroleum company service channel dredged from the Intracoastal Waterway to provide access to a drilling site 13. Mansfield Channel 14. Three theories of barrier island origin 15. Sketches representing several stages in the history of the southern Texas coast 16. Sea-level changes during the past 18,000 years, as interpreted by various authors 17. Spit accretion 18. Cross section of central Padre Island near beach mileage marker 30 19. Net shoreline changes along Padre Island National Seashore based on time periods of various lengths between 1862 and 1975 20. Waves approaching shoreline at an oblique angle, producing longshore currents 21. Direction of littoral, or longshore, drift along a straight shoreline 22. Effect of the concave Texas Gulf shoreline on directions of littoral drift 23. Geologically effective winds (predominant winds) on Padre Island 24. Jetties at Mansfield Channel 25. Little Shell Beach sediment, consisting primarily of shells of the small clam Donax 26. Big Shell Beach sediment, consisting primarily of abraded shells of large clams 27. Characteristics of a wave that define wave steepness 28. Waves breaking along offshore submerged sandbars (wave breakpoint bars) 29. Swash bar on a shell beach on central Padre Island 30. High, partially eroded berm of a steep, central Padre shell beach 31. Observation trenches dug along the gulfward edge of berms on Big Shell Beach 32. Beach cusps 33. Beach cusps near Malaquite Beach 34. Closely spaced cusps on a steep, central Padre shell beach 35. Examples of salt-spray-tolerant plants that help trap and hold sand to form stabilized dunes along the Gulf shoreline 36. Well-vegetated portion of central Padre Island in the vicinity of grids H-11, J-11, and K-11, plate I 37. Sparsely vegetated segment of Padre Island immediately north of Mansfield Channel 38. Generalized diagram depicting the sun as the energy source behind the wind 39. General characteristics of dunes and common dune types, shown in relation to wind direction 40. Active back-island dune on Padre Island 41. Deflation trough or flat formed along the trailing edge (windward side) of an active dune 42. Diagrammatic cross section of deflation troughs and interlying stabilized ridges compared with a graph of rainfall 43. Generalized sketch of an active dune and related deflation troughs 44. Aerial photograph of active dunes shaped by southeasterly winds 45. Oblique, low-level aerial photograph of active dunes shaped by northeasterly winds 46. Active dunes in a state of transition as they respond to changing wind directions 47. Lagoonward migration of sand in response to onshore (southeasterly) winds 48. Aerial photograph showing the direction of elongation of active dune fields in relation to their net direction of migration 49. Movement of active dunes with respect to major wind directions 50. Comparison of the distribution of island environments as they appeared in (a) 1956, (b) 1967, and (c) 1975 51. Active longitudinal dune on the lagoon side of Padre Island 52. Ripple marks showing sorting or segregation of sediments by the wind 53. Ripple marks in which flakes of shell material have been sorted or segregated from finer grained quartz sand by the wind 54. Trench dug in hurricane washover channel on Padre Island 55. Alternating layers of sediment, composed predominantly of quartz sand and shell fragments, in a fore-island dune on Padre Island 56. Trench dug behind a small dune (vegetated with sea oats) located near the beach on Padre Island 57. Close-up view of trench shown in figure 56 58. Dune crossbedding, Padre Island 59. Truncated crossbedding exposed on nearly horizontal surfaces windward of an active back-island dune on Padre Island 60. Sequence of events that can produce crossbeds dipping in different directions 61. Aerial photograph of washover channels along central Padre Island that were activated by storm surge accompanying Hurricane Beulah 62. Sketch of washover channels and washover fans, shown in relation to other natural environments on central Padre Island 63. Natural shell "pavement" lagoonward of the fore-island dunes on Padre Island 64. Seawall on south Padre Island, south of the National Seashore 65. Northern end of pedestrian beach, along which vehicular traffic is not allowed 66. Trails worn in fore-island dunes by pedestrians 67. Experimental fore-island dune ridge 68. Bulldozer scraping windblown sand off the paved parking lot at Malaquite Beach 69. Tongues of sand blown by onshore winds onto a road near Malaquite Beach 70. Road rerouted because of migrating dunes 71. Natural gas wellhead threatened by burial under windblown sand 72. Methods used to stabilize loose sand and prevent it from being blown by the wind 73. Shell beach 74. Generalized profile from upper shoreface to fore-island dunes 75. Beach profiles recorded June 17-18, 1975 76. Malaquite Beach, typical of north Padre beaches, having a flat profile and broad, shallow cusps 77. Coppice dune field lying between the beach and the fore-island dune ridge 78. Broad coppice dune fields in the southern part of the National Seashore near Mansfield Channel 79. Fore-island dune ridge of central Padre Island, as viewed from the surf zone 80. Fore-island dune ridge at one of its widest points 81. Heavily vegetated barrier flat supporting various grasses and small shrubs 82. Sparsely vegetated barrier flat 83. Novillo, the northernmost line camp constructed by Pat Dunn for cattle ranching on the island during the late 1800's and early 1900's 84. Park Road 22, which cuts through stabilized blowout dunes just north of the Bird Island Basin road intersection 85. Hurricane washover channel at the 35-mile beach marker 86. Wind-deflation flat at the trailing edge of a back-island dune field 87. Washover fan spreading onto a deflation flat 88. Ponds occupying long wind-deflation troughs, which parallel back-island dune fields 89. One of the marshy ponds that have developed in deflation flats left by fore-island blowout dunes 90. Blowout complex that originated at the dune ridge, where stabilizing vegetation had been destroyed and loose sand was free to blow out 91. Back-island dune field including several large, shifting dunes 92. Trench dug on a wind-tidal flat, showing the alternating layers of sand (light layers) and clay (dark layers) 93. Wind-tidal flat covered by extensive algal mats 94. Gypsum rosettes 95. South Bird Island, a natural island in Laguna Madre 96. North Bird Island 97. Lagoon-margin sand 98. Large sand waves and ripples on lagoon-margin sand exposed during very low tide 99. Small cliff at the edge of the barrier flat, eroded by high wind and storm tides 100. Lobes of lagoon-margin sand oriented southward, in the direction of prevailing lagoonal currents 101. Subaqueous grassflat in Laguna Madre 102. Lagoon grassflat exposed during low tide 103. Dead shoalgrass that has been washed onto a wind-tidal flat, dried in mats, and bleached white by the sun 104. Rows of bleached shoalgrass marking varying tide levels on the wind-tidal flats and reworked spoil 105. Middle Ground, an area of wind-tidal flats and shallow grassflats 106. Muddy sand on the center bottom of Laguna Madre, just south of the Land-Cut Area 107. Dredged spoil along the Intracoastal Waterway 108. Petroleum company facilities on the northern part of the Seashore 109. Historical sites on Padre Island 110. South Texas 111. Route for north Padre field trip 112. Padre Island National Seashore entrance on Park Road 22 (Observation Point 1) 113. Beach at north beach access road (Observation Point 2) 114. Effects of beach traffic on vegetation near north beach access road 115. Trailhead of the Grasslands Nature Trail (Observation Point 3) 116. Barren, active blowout dune near the Grasslands Nature Trail 117. Shells of the oyster Crassostrea, dredged from nearby bays and placed on barren dunes on the east side of Park Road 22 to prevent loose sand from blowing across the highway (Observation Point 4) 118. Marshy ponds occupying wind-deflation troughs (Observation Point 5) 119. Exposed roots of live oaks 120. Large, elongate dune in a back-island dune field (Observation Point 6) 121. Grassflats, environments of very high biological productivity, lying in calm water just beyond the lagoon-margin sand (Observation Point 7) TABLE 1. Characteristics of Hurricanes Carla, Beulah, and Celia, as measured at Texas stations PLATE I. Geology and natural environments of Padre Island National Seashore, Texas (omitted from the online edition)
state/tx/1980-17/contents.htm Last Updated: 28-Mar-2007 |