Dr. Jeff Marshall - Research

 

Central America and southern México

 

Research Project:

Geomorphology and physiographic provinces of Central America and southern México

(Chapter 3 in Central America: Geology, Resources, and Hazards, ed. by Bundschuh & Alvarado)

 

 

 

Map of the physiographic provinces of Central America as defined in this study. Solid lines indicate province boundaries. Numbers on map refer to the list of physiographic provinces at right. Yucatán platform and Chortis highlands sub-regions: a, Northern pitted karst plain; b, Southern hilly karst plateau; c, Petén karst plateau and lowlands; d, Eastern block-faulted coastal plain; e, Central Chortis plateau; f, Western rifted highlands; g, Eastern dissected plateau; h, Honduran borderlands. Digital elevation model derived from NASA Shuttle Radar Topography Mission (SRTM) image PIA03364.

Book Cover:  Bundschuh, J. and Alvarado, G., eds., Central America: Geology, Resources, and Hazards, Taylor and Francis, London.

For complete table of contents and publisher information click on the links below.

 


 

Project Overview:

 

Several years ago, I was invited to write a book chapter on the geomorphology of Central America for a new comprehensive volume entitled Central America: Geology, Resources, and Hazards, edited by Jochen Bundschuh and Guillermo Alvarado (published in 2007 by Taylor & Francis).  For this project, I decided to write a general review of geomorphic research in Central America, including my own work in Costa Rica.  In preparing this chapter, I encountered an astounding array of geomorphic research on many topics, but soon realized that no one had previously defined a system of regional physiographic provinces for Central America.  I decided that this would be the primary contribution of this chapter and would serve as a structure for organizing my review of prior work.  The figure above shows my map of the newly defined physiographic provinces for Central America.  The following paragraphs are excerpts from the book chapter introduction.

 

Book Information:

 

Central America: Geology, Resources, and Hazards, 2007, (Volumes 1 & 2), Bundschuh, J. and Alvarado, G., Taylor and Francis, London.

 

Table of Contents

Taylor & Francis Publishers

 

Geomorphology Chapter Overview:

 

Chapter 3:  The Geomorphology and Physiographic Provinces of Central America

 

Jeffrey S. Marshall

 

“We have been sailing placidly along the coast…all day - a broad, low land, densely clad in a green, tropical vegetation…. In full view are three noble mountains - tall, symmetrical cones, with sides furrowed with wrinkle-like valleys veiled in a dreamy, purple mist that is charming to the eye, and summits swathed in a grand turban of rolling clouds. They say these are volcanoes, but we cannot see any smoke. No matter - it is a fairy landscape that is very pleasant to look upon.”  Mark Twain, December 1866, letter written aboard the steamer Columbia offshore of Guatemala, published in the San Francisco Alta California, March 15, 1867

 

Central America encompasses an intricate mosaic of dynamic landscapes shaped by a wide range of Earth surface processes. Few other regions worldwide exhibit a comparable magnitude of geomorphic diversity. Along the length of the Central American isthmus, highly variable tectonic, lithologic, and climatic domains are superimposed across a small land area (0.4 % of Earth’s total land surface). The resulting physiography is characterized by a heterogeneous array of geomorphic provinces, each featuring a distinctive landform assemblage that preserves a unique history of landscape evolution.

 

Over 1500 km in length, Central America reaches from the rugged Maya highlands of Guatemala in the north, to the humid coast ranges of Panama’s Darién isthmus in the south. This narrow land bridge links the two American continents and forms a critical divide between the Pacific and Atlantic ocean basins, varying in width from less than 100 km at the Panama Canal, to over 400 km across the interior highlands of Nicaragua and Honduras. From towering volcanic peaks (>4000 m elevation) to jungle-shrouded alluvial lowlands, and from rugged tectonic shorelines to passive-margin lagoons, Central America embodies a geomorphic microcosm of remarkable diversity.

 

As a whole, the Central American isthmus forms a geologically tenuous land bridge that links the two American continents and creates a topographic divide between the Atlantic and Pacific Ocean basins. This narrow landmass plays a vital role in directing the ecological evolution of the Americas, and may also profoundly influence ocean circulation and global climate. During the Cenozoic, a diverse array of landscapes has developed along the isthmus in response to dynamic interactions between regionally variable rock types, complex plate-boundary tectonics, and an energetic tropical climate. Central America therefore serves as a unique laboratory for the study of a wide range of geomorphic processes and consequent pathways of landscape evolution.

 

This chapter explores the regional geomorphology of Central America and defines a system of physiographic provinces that characterizes the overall landscape diversity of this dynamic region. The chapter is organized into sections that provide an overview of the characteristic landforms and geomorphic processes that define each of the physiographic provinces. The first half of the chapter looks at the geomorphic provinces of northern Central America, and the second half examines those of southern Central America. Each section provides a brief review of current geomorphic research within the physiographic provinces. Due to the wide range of possible topics, it is impractical to cover every aspect of these diverse landscapes. The discussion is therefore limited to a subset of critical topics that provide a general flavor for the regional geomorphology of Central America. Several of these topics are explored in greater detail in the four chapters that follow: Volcanism and volcanic landforms (Chapter 4), Karst landscapes (Chapter 5), Glacial geology and geomorphology (Chapter 6), and Coastal morphology and coral reefs (Chapter 7).

 

 

Pre-print of Chapter 3 (draft version):

 

Marshall, J.S., 2007, Geomorphology and Physiographic Provinces of Central America: in Bundschuh, J. and Alvarado, G., eds., Central America: Geology, Resources, and Hazards, Taylor and Francis, London, p 75-122.

 

[PDF file: 2.9 Mb]

 

Images: 

Project illustrations

 

 


 

Back to:

Research page

Home page