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The Wayƒarer
The Mountain
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THE GEOGRAPHICAL REGIONS
The Coastal Plains Region, Texas

The Western Gulf Coastal Plains Ecoregion Go Down Go Back
The Western Gulf Coastal Plains ecoregion is a geographical area almost entirely along the Gulf Coast of the United States, primarily encompassing the coastal plain of Texas, extending into parts of Louisiana and reaching into northeastern Mexico, characterized by relatively flat topography and predominantly grassland vegetation as its natural potential vegetation. The Western Gulf Coastal Plains is often considered a part of the larger "Gulf Coastal Plains" ecoregion.
The Gulf Coast
The Gulf Coast has been referred to as America′s Third Coast, and Texas has 367 miles of this third coast. Here in Texas, their are warm waters, seaside restaurants, great camping and small beach towns unlike any you will encounter on the the other two coasts, (the Eastern and Western Seaboards). Yes, the simplicity of Texas beaches far surpass all others for any getting away for some self time.
However, of late, this beauty and wonder that belong to these warm water beaches has become the destination location to an every growing number of people. And we all know what happens to a beautiful spot that becomes overused. Still, despite the crowds, there are still places to find a spot to enjoy the creation.
One of my favorite locations is Padre Island national seashore.
Too, the Gulf Coast of Texas is replete with inland bays, great for all those activities people do on or near water, including beaches. Again, I have been know to stop at Magnolia Beach a time or two.

Western Gulf Coastal Plains Information:
Description:
The total area of this ecoregion is just under 30,000 square miles. The specific areas include a number of barrier islands, and the resacas or natural levees of the Laguna Madre. Too, this coast is vulnerable to tropical storms that can seriously damage ecoregion habitats.
This coastal plain in Louisiana is often called the Cajun Prairi; in Texaa, is is know a the Coastal Prairie; and in Mexico, it is known as the Tamaulipan pastizal.
Less than 1% of the ecoregion remains in pristine condition, almost entirely in Texas, while most of the coast has been converted to farmland, including rice paddies, grazing land, or urban areas including Houston, Texas. Estuaries and other coastal wetlands are better preserved than the prairie and indeed the protected areas of the coast are mainly sanctuaries for waterbirds.
Climate
From Southwest Louisiana west to the Upper Texas coast, the climate is wet humid subtropical, featuring significal annual precipitation. The climate becomes more arid farther south along the Texas coast into northeastern Mexico, though precipitation totals still remain high enough for the humid subtropical classification.
Unlike the Southern Inland Plains ecoregion which has already been engulfed within Dry side of the climate divide, the Western Gulf Coastal Plains ecoregion still receives from 27 to 30 inches of rain per year, which is more than enough to make a difference from the adjacent ecoregion, the Southern Inland Plains. In fact, there are more overcast days along the coast that makes it just more humid that in those inland areas.
Flora
The natural habitat of the area is a mix of tallgrass prairie similar to those found in inland Texas, with Indiangrass (Sorghastrum nutans), big bluestem (Andropogon gerardi), little bluestem (Schizachyrium scoparium), and switchgrass (Panicum virgatum) the primary tallgrass species that are typical of the coastal prairie, with several other shorter grasses and many herbaceous and woody species.
In the wetter climate covering the zone from Southwest Louisiana west through the upper Texas coast, these bottomlands contain many species typical in forests elsewhere across the Southern United States, such as the southern live oak, bald cypress, magnolia, loblolly pine, post oak, and southern hackberry. Farther south, from the lower one third of the Texas coast and through the Tamaulipan stretch, the drier climate supports shrubby areas of honey mesquite (Prosopis glandulosa), huisache (Vachellia farnesiana var. farnesiana), lime prickly-ash (Zanthoxylum fagara), and Texas persimmon (Diospyros texana).
Fauna
This coast is rich in wildlife, and 700 species of birds, animals and reptiles have been counted here, although many are now threatened or endangered.
Birds
This coast is a critical habitat for both species of the prairie-chickens but paticullary the Attwater′s prairie chickens (Tympanuchus cupido attwateri), over one million of which inhabited the prairie in Texas and Louisiana in the 19th century, but extreme reduction of their habitat put them on the U.S. endangered species list in 1967.
Another endangered bird of the coast is the whooping crane (Grus americana). Many species of wading birds, shorebirds, and other waterbirds are abundant, such as the sandhill crane, now numbering world wide at about 650,000 individual birds.
Birds in the Mexican part of the region include Morelet’s seedeater (Sporophila morelleti), red-billed pigeon (Columba flavirostris), brown jay (Cyanocorax morio), Neotropic cormorant, white-winged dove (Leptotila verrequxi) and Audubon's oriole (Icterus graduacauda).
Mammals
Mammals of the area include bobcats, collared peccary, white-tailed deer, eastern cottontails, with ocelot (Leopardus pardalis), Gulf Coast jaguarundi (Puma yagouaroundi cacomitli), southern yellow bat (Lasiurus ega), and Mexican spiny pocket mouse (Liomys irroratus) more abundant in Mexico.
Amphibians and Reptiles
Rancho Nuevo beach in Tamaulipas and along the Texas coast are the only nesting sites in the world for the Kemp's ridley sea turtle (Lepidochelys kempii) while other herpetofauna of the southern part of the ecoregion include Río Grande chirping frog (Eleutherodactylus cystignathoides) and Mexican white-lipped frog (Leptodactylus fragilis).
Location:
Coordinates:
Elevation: feet
Geographical Region: Coastal Plains

The Ancients
Ancient Steps:
One of the very first indigenous people that I ever learned about who lived along the Texas coastal lands were the Karankawa native Americans, extinct since about 1860, who were a nomadic tribal group that traveled in bands of less than 100. They fished and hunted the upper Texas Gulf Coast from Galveston bay to as far south as Corpus Christi bay, and inland for about 100 miles.
What I had learned about these indigenous people is that they were known for cannibalism. Warfare was a fact of life for the Karankawas, and they practiced a ceremonial cannibalism prior to the eighteenth-century that involved eating the flesh of their enemies. That custom is believed to be widespread among most Texas tribes during that time and involved consuming pieces of the flesh of dead enemies as the ultimate revenge or as a magical means of capturing the enemy′s courage.
First Wayƒarer
First Migration (The Algonquian Cultures)
The Karankawa indigenous people were of the first migration and concentrated in southern Texas along the coast of the Gulf of Mexico, largely in the lower Colorado River and Brazos River valleys. They consisted of several independent seasonal nomadic groups who shared the same language and much of the same culture.
There is a general misconception that these indigenous people migrated north from areas in or near the Caribbean islands. The truth of the matter is that the Karankawa language is a dialect of the Coahuiltecan Language, which decedented from Diklah, son of Joktan.
Furthermore, much of what has been written about the Karankawa, it has been said, was composed by their enemies. The claim concerning their cannibalism was a lie propagated by the Spanish in retaliation to the Karankawa not wanting to convert to Catholicism.
Second Migration (The Uto-Aztecan Cultures)
The only Uto-Aztecan language indigenous people in Texas were those primarily in west Texas, which were the Jumano Cultures including the Caquate, Tanpachoas, and Tomoacas which only lived along the upper Rio Grande river valley.
There was also a separate tribe which lived in the Great Plains along the upper Colorado River, but the the Athabascan, primarily the Lipan Apache took over most all of the plains region.
Third Migration (The Athabascan Cultures)
The Athabascan Speaking People
The Lapain indigenous people were of the third migration and settled in the inland areas on and near the edge of the Edwards Plateau after moving down from the upper Great Plains region in the Texas panhandle .

The Earth
Geological:
Waterways:
Rivers:
Mouth: Gulf Of Mexico
Brazos River: Nolan River Little River, Bosque River, Paluxy River,
Colorado River: Pedernales River, Llano River, San Saba R., Concho R.
Guadalupe R.: S. Antonio R., Medina R., S. Marcos R., Blanco R., Comal R.
Lavaca River: Navidad River
Neches River: Angelina River
Nueces River: Frio River,
Sabine River
San Bernard River
San Jacinto River
Trinity River: Big Sandy Creek
Rivers and Tributaries
Mouth: (Atchafalaya River)
Red River: Big Cypres Bayou, Sulphur River, Washita, Wichita River,
Prairie Dog Town Fork Red River
Mouth: (Arkansas River)
Canadian River
Seas and Seashores:
Sabine Pass (Civil War) Battleground State Historic site (29.731167, -93.874842)
Wonders:
Parks:
Padre Island National Seashore.

The Modern Man
Lighthouses
Port Isabel Lighthouse

The Steps
Pathway Journeys:
Steps Afoot
Footpath Journeys:
Texas Footpath Journey Index
Steps Afield
Roadpath Journeys:
Texas Roadpath Journey Index

The Appendixes
Campgrounds:
Texas Campground Index
Region Campgrounds
Altair Boat Ramp parking under Alternate US 90 at Colorado River
Brazos Bend State Park an hour southwest of Houston
Galveston Island State Park in the west end of the Island
Goliad State Park
Goose Island State Park near Rock Port, TX
Lake Corpus Christi State Park, IH 37 exit 36, near Mathis, Texas
Magnolia Beach west side of Lavaca Bay
Malaquite Campground on the coast in Padre Island national seashore
Mustang Island State Park just east of Padre Island
Sea Rim State Park near Port Author, Texas

The 2024 Journey, Western Gulf Coastal Plains Ecoregion Go Down Go Up
(Day 980 TN) 44deg;F. 6:30 am, Overcast
Winter Sojourn, Day 26
Overnighting in a parking lot
Just ten miles, as the crow flies, north of SpaceX Launch Facility is where the Queen Isabella Causeway bridge and Texas State highway (SH) 100 leave South Padre Island and crosses the Laguna Madre to the South Texas mainland, all in only 2.75 miles. As you come close to the mainland, you will begin to see the Port Isabel Lighthouse which is near the point where the causeway bridge arrives in Port Isabel, and as you arrive on the mainland, you will see the lighthouse looming all of its 82 feet above its base and just to the north of SH 100. The lighthouse was built in 1852 as an aid to navigation. About sixty-two miles west of South Padre Island,
If you continue west on SH 100 for another eight miles, you will see the entrance to Laguna Atascosa National Wildlife Refuge, which is a habitat for wintering waterfowl and premier bird-watching destination. Some of the species include redhead ducks, Aplomado falcon, Painted buntings,
After passing the refuge, there will be another sixteen miles will before arriving at the intersection of IH 69E, a total of just over 27 miles from South Padre Island. Turning north onto IH 69E, enter the interstate and drive another ten and a half miles and take exit 26A, Lincoln Avenue. On the right will be Harlingen, Texas and access to a lot of places to overnight park, eat, sip coffee and etc. This is a place that I have been frequenting for more than twelve years since I have been living in my vehicle.
This year, For over a week, here in Harlingen, Texas, it has been necessary to keep my windows closed because of the constant rain that has been coming down. Even this morning, I noticed that there was a slight leak above the sliding side door which caused my my bedding to become wet. No, I do not like the wet side of this continent. I would rather stay dry side in order to avoid the rain entirely.
The Coastal Plains Region
The Western Gulf Coastal Plains Ecoregion
(m2cont-nam-12-tx-12d-stx-2024-0122.0635) After a long night of rain, I awake to start my day

The Divide called: Climate Divide
When leaving Harlingen, Texas to drive west the one hundred miles inland to Falcon State Park, I always come to the edge of the Climate Divide.
No, this divide is not an imaginary line, at least not in this location because there is a definitive line shown by the end of the cloud cover and the beginning of the blue desert skies.
The Coastal Plains Region
The Western Gulf Coastal Plains Ecoregion
(m2cont-nam-12-tx-12d-stx-2024-0105.1125) Driving out from under the cloud cover

The 1968 Journey, Western Gulf Coastal Plains Ecoregion Go Down Go Up
Growing up in Texas
When I was a baby, my father graduated from Tulane University with a Chemical engineering degree. Not long after that, my father received a good job offer with one of the oil refinery companies in Texas, so, after accepting the job offer, my parents moved from New Orleans, Louisiana to Borger, a town in the north Texas panhandle. Once that oil company saw the potential that my father had, he was offered a position at the Pasadena refinery. Apparently, it was a very good offer because he accepted it and subsequently moved his ever-growing family to a new home in Pasadena, Texas. Later, the home that our family finally settled into was only a five minute drive from his office. This is where our family remained for many years, all of the eight children growing up and going to the Deer Park, Texas school district.
Then, when I had graduated from my grade school incarceration during then of May 1968, my story began. What I mean by "my story began" is that upon finishing school, I was only then able to step out upon other Journeys, which were separate pathways that began a time in my life during which I could and did impart upon one of the first of many Journey On adventures.
Early Journey On
Shortly after graduating in 1968, likely in the winter of 1968 - 1969, I began to drive some forty odd miles from my home in Pasadena south along the then new IH 45 to the island city of Galveston where I would participate in the sport of surfing on the waves coming in from the Gulf of Mexico.
This being the first time that I was to see this island city, and I was amazed upon seeing the massive seawall and the great piers that held the huge motels, one of which had some great memories from my early adulthood. In fact, when I was later married, I took that new wife to the Flagship Hotel for our honeymoon trip. However, this woman, after about seven years married to me choose to get a divorce and go her separate way.
The Coastal Plains Region
The Western Gulf Coastal Plains Ecoregion
The Great Galveston Hurricane
The storm that hit Galveston on September 8, 1900 was a Category 4 hurricane and was called the Great Galveston Hurricane because the naming conventions we now have did not exist during the early part of the 1900s.
The Great Galveston Hurricane resulted in an estimated fatalities of between 6,000 and 12,000 people. Other estimates state that there were 8,000 people killed. Historically, the Great Galveston Hurricane was and still is the deadliest natural disaster in all of United States history.
That storm ravaged Galveston island, broke houses apart houses, carrying many further inland, causing untold havoc. Many of the inhabitant of the island died, most from drowning. This turn of the century devastation led to the downfall of Galveston as a major port on the Gulf of Mexico and the allowed for the subsequent rise of the port of Houston. However, those of the islanders who survived refused to abandon their homes, and they began to develop plans began shortly after this devastation to prevent any such tragedy from ever reoccurring again in the future.
The Plan
The plan to protect Galveston Island and keep future storm surge waves from overcoming the city of Galveston, Texas was composed of two separate parts.
The First part of the plan involved raising all structures to a specified elevation and then raising the elevation of the land by pumping in sand under the structures. Because homeowners had to incur the cost of raising their homes, some opted to fill their ground floors with dirt and live on the second floors and above. Still, the raising of all structures more than a full story higher was quite an accomplishment, especially with the current technology available.
The Second part of the plan required for the construction of a 10.3 mile long seawall to be built along the Gulf of Mexico side of the island. This portion of the plan to protect the island and keep future storm surge waves from overcoming the city involved building a 17-foot high wall. Of these two parts, the seawall proved the less ambitious.
The Coastal Plains Region
The Western Gulf Coastal Plains Ecoregion The Coastal Plains Region
The Western Gulf Coastal Plains Ecoregion
The Raising Work
Starting in 1903, about three years after the devastating 1900 storm hit Galveston, Texas head on, the entire city was systematically raised, which raising work continued for eight years through to 1911. The goal of the raising work: to raise the entire city: the homes, the businesses, the churches, the streets, the sewers, the yards... The entire city was to be raised more than 2000 structures and more than 15 million cubic yards of sand was pumped from the bed of the Gulf of Mexico to raise the elevation of the ground under and around all of the raised structures.
This raising work was accomplished with the use of a very large number of hand crank jack screws simultaneously lifting each structure to the new elevation for each area of the city. Depending on where each location was in relation to the Gulf of Mexico, the structures closest to the gulf (at the seawall) would be raised a little more than 17 feet and locations slightly further north of the gulf would be raised slightly less than the 17 feet. The amount each structure would be raising would decrease depending how far from the gulf that structure was and the amount the would be raised would go down to about 8 feet on the extreme northern side of the city.
This raising of the city included roughly about 500 city blocks, and the eventually resulted in making the elevation at the top of the seawall about 17-18 feet above sea level, while the elevaion on the inland side (north side) of the city would be about 8 to 10 feet above sea level. This first part of protecting the island which called for raising the structures and land area within the city of Galveston was not the only thing that was done during the years of rebuilding, but during the same time, the construction of the Seawall was accomplished.
The Seawall
Despite the city of Galveston having a population of more than 44,000 prior to the Great Galveston Hurricane of 1900, Galveston Island (located in the Western Gulf Coastal Plains ecoregions of Texas), 1 was then no more than a sandbar in the Gulf of Mexico, having an elevation of only a few feet above sea level, much like Padre Island is now.
Then, during the rebuilding work of the city of Galveston, Texas, the second part of the plan to protect the city from future storm surge waves from inundating the city was to build a concrete seawall along the entire south edge of the city. This seawall was constructed up to the height of 17.5 feet along the gulf side of the city, with a base thickness of 16 feet wide at the bottom of the seawall to a thickness of 5 feet wide at the top of the seawall. Too, the gulf facing seawall streches for some 10.3 miles along the city of Galveston, Texas.
The New Elevation
The land immediately behind (north of) the seawall was then raised to the same elevation of the seawall and thus raised the elevation of Galveston, Texas to about 17 feet above sea level. Attached directly to this Seawall is a 10 to 15 foot wide sidewalk promenade which expands the width of the Seawall at the top of this historic seawall. Thus, the new elevation began with the top of the seawall, continued across a 10-15 foot wide promenade directly nest to the seawall, and then continues across Seawall Boulevard, which, by the way brings the total concrete stucture, (including the top of the Seawall) to the width of about 75 feet. This entire concrete structure is atttached to the Seawall and resides at the same elevation of the top of the Seawall, about 17 feet above sea level.
This amounts to a massive concrete corridor space, running alongside the famous 16-foot-thick base of the historic seawall.

1  
The Texas gulf coast plains are a low elevation region with very little elevation gain throughout. I first learned about this while living in the city of Pasadena, Texas where I grew up and did my incarceration during the grade school years. The elevation of Pasadena, Texas is about 25 feet above sea level, dispite it being over a forty mile drive inland from Galveston, Texas.

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