ArticlePDF Available

Abstract and Figures

In the desert environment of south-west Jordan thick sequences of continental sandstones of Cambrian-Ordovician age support spectacular scenery, comparable with that of the Colorado Plateau of south-west USA or the central Sahara and similar in many aspects to the Danxia landform of southern China. Dissection of a sandstone tableland has given rise to numerous inselbergs and large mesas, rising from the sand-covered desert floor. The height of the hills varies from a few tens to 500-700 m in the Wadi Rum area, whereas their slope shapes are controlled by lithological properties of particular sandstone units. Rock walls of the sandstone inselbergs are subject to frequent rock falls and rock slides and host an impressive array of tafoni and honeycombs due to selective weathering, as well as a number of rock arches. Lithological differences within the sandstone sequence are crucial controls on the shape and evolution of rock slopes, exerting the influence via contrasting patterns of weathering and slope failures. The presence of ferruginous layers in the Umm 'Ishrin Sandstone is of major importance and explains the fundamental morphological differences between the otherwise similar Umm 'Ishrin and Disi sandstone units. © 2014 Faculty of Geographical and Geological Sciences, Adam Mickiewicz University.
Content may be subject to copyright.
QUAESTIONES GEOGRAPHICAE 33(3) • 2014
SANDSTONE GEOMORPHOLOGY OF SOUTH-WEST JORDAN,
MIDDLE EAST
Piotr Migoń1, Andrew Goudie2
1
2


Migoń P., goudie A

AbstrAct:







    
  

Key words:
Piotr Migoń, Instytut Geograi i Rozwoju Regionalnego, Uniwersytet Wrocławski, Pl. Uniwersytecki 1, 50-137 Wrocław,
Poland; e-mail: piotr.migon@uni.wroc.pl
Andrew Goudie, School of Geography and the Environment, University of Oxford, South Parks Road, OX1 3QY Oxford, Great
Britain; e-mail: andrew.goudie@stx.ox.ac.uk
Introduction





 
        
 
     


   




   
 
        


 

120 
     
    


    
      
      

      

       
     






 
      

     
     


    
 

       

    
        
    

    

Geographical setting
     







      
    



     

     
      


     
      
 

 
  
    

 
       

 
      


  



2).
 
      



 121
      




Landform diversity and its relationship
to geology
Geology






    

      


     




  
       


  


    
    


  
         
   

        
      
      


  

   

 
     








Landform diversity





     

      
       
  
    
    

   
   
  

       

       


     
      
      
      


       

   
     
     
  
122 
        
      

  
    
     

     
     
      
      
      
      
      

       
     

       

     

    


       
  

      


      


    
         
     

      

       
      












 123
       

  





  

    
       
  
      
     



     
    

      
      
       





      

     
     
 

    

    
   
    
  




       

Rock slope failures and patterns
of slope evolution



   
       


     
     


       
    
     
  



    





124 


    







       

       

      

      
      



   



      
     




 
      

    





 125
      


    
     
     
     

        

    
      
       
      

Conclusion
     

     
     
    
        
     

      
    
     

    



     
  

     
     
 




    
     
      
   
  

    
      
 
   
     

     
     
      


     
  


References
The geology of the Jabal Umm Ishrin area
(Wadi Rum)
      
   Mitteilungen der
Fränkischen Geographischen Gesellschaft

       
Geolines

        

Neues Jahrbuch für Geologie
und Paläontologie, Monatshefte

 The Natural Arch and Bridge Society website 
 



Zeitschrift für Geomorphologie N. F.



126 
    Karst and
Pseudokarst in Northern Australia. Report on the eld study
of June-August 2008    

        

 Koedoe 


Sandstone Landscapes
       
   First International Symposium on Danxia
Landform. World Danxia. The 1st Collection 

       
      
Zeitschrift für Geomorphologie N.
F.
       
  
Sedimentary Geology
  



Earth and Planetary Science Letters
       
 
   
Rekonstrukcja dy-
namiki procesów geomorfologicznych formy rzeźby i osady.
   
     



Journal of Arid Envi-
ronments 

Palaeogeography, Palaeocli-
matology, Palaeoecology

Palestine
Exploration Quarterly
Danxia Geomorphology of China and Its Pro-
gress in Research Work   

  The geology of the Al Quwayra area 

Geologischer Führer durch das Elbsandsteingebirge.



Rock Weathering and Landform Evo-
lution

   
Journal of Geological Society London
     
     Earth Surface
Processes and Landforms

Journal of Ge-
ology
       Sandstone
Landforms
        First
International Symposium on Danxia Landform. World Danx-
ia. The 1st Collection   

... This strongly suggests causal relationship. The origin of rounded hillslopes was more often addressed in respect to sandstones (Ollier and Tuddenham, 1961;Bradley, 1963;Young, 1986Young, , 1987Young et al., 2009;Migoń and Goudie, 2014), but is perhaps even more relevant to conglomerates as other hillslope shapes, common in sandstones, are rather infrequent and sharp edges are rare. It is important to note that these curved shapes are not necessarily related to sheeting joints, which are actually quite rare in conglomerates. ...
... Rather, the origin of curved shapes in sandstones is attributed to dominant grain-by-grain disintegration and not to detachment of larger rock pieces delineated by joints (Young, 1986;Howard and Kochel, 1988;Young et al., 2009). In the sandstone landscape of south Jordan iron-rich intercalations in one sandstone member give rise to distinct rims, ledges and benched slopes, whereas another one, lacking iron inliers, develops perfect convex hillslope shapes (Migoń and Goudie, 2014). Extending this concept to conglomerates, one can replace grain-by-grain breakdown by clast-by-clast disintegration, as already indicated by Young et al. (2009). ...
... Comparative studies of sandstone topographies worldwide indicate two major mechanisms of rock breakdown and slope development Young et al., 2009;Migoń and Goudie, 2014). One is grain-by-grain breakdown which results in smooth slope shapes and curved profiles, typically convex. ...
Article
Conglomerates are widespread clastic rock, often occurring in thick successions and supporting complex geomorphological landscapes. Yet, by contrast to some other rock types, little systematic work has been done on geomorphology of conglomeratic terrains, major geographical gaps exist, and no review has been offered up to now. This paper partially fills this gap and provides an overview of characteristic landforms, landscape types and geologic controls present in areas built of conglomerates. Distinctive landforms developed in conglomerates include bedrock cliffs and overhangs, domed hills and hilltops, crags, slots and clefts, tafoni, caves and various karst features. They combine into specific landform assemblages of dome clusters, dissected plateaus and cuestas, stepped hillslopes and conglomeratic badlands if lithification of sediment is poor. Some dissected plateaus and dome clusters represent spectacular morphology, awarded the status of UNESCO World Heritage (China Danxia, Meteora, Kata Tjuta). A variety of geological controls is identified and presented, including composition of conglomerate packages, their thickness, jointing patterns, presence of sandy and clayey intercalations, as well as the style and magnitude of regional uplift. Clast-by-clast breakdown is identified as a principal mechanism of rock disintegration, analogous to grain-by-grain disintegration pattern of many sandstones. This explains striking similarities between some sandstone and conglomeratic sceneries and the common presence of rounded shapes. In the closing part of the paper research avenues for the future are suggested. Both regional studies, aimed at the complete inventory of conglomeratic landforms, as well as detailed insights into the nature of bedrock control at the variety of scales are recommended.
... Finally, 27 cisterns have extant lime-based mortars to waterproof their walls and prevent water leaks due to the high absorption coefficient of the Disi Sandstone that shapes the landscape where Sela is located (Migón and Goudie, 2014). They are mainly preserved in the storage chambers, although they can also be found lining the entire structure. ...
... Fig. 14 illustrates how the hydraulic installations are distributed in different areas with elevations ranging from 878 to 870 m amsl (areas H and G) to 850-840 m amsl (areas D, E, and I). As Migón and Goudie (2014) indicated, the sandstone's permeability and the scarce vegetation in the area would produce a high water infiltration into the ground. However, during episodes of high-intensity rainfall, the infiltration rate was probably reduced, increasing water runoff (Bender, 1974;Salameh et al., 2018). ...
Article
Full-text available
The efficient management of water resources to supply the needs of societies in territories where water is a scarce and limited resource has been essential throughout time. The site of Sela on the southern Transjordan plateau is unique for understanding water management in this semi-arid area. The analysis of hydraulic installations has allowed us to characterise its hydro technology and spatial distribution in the settlement. To this end, the hydraulic facilities have been identified, documented, and analysed in detail through two archaeological surveys (2015 and 2016). Spatial analysis has been carried out by preparing extensive 2D planimetry and 3D reconstructions. The results obtained have made it possible to reconstruct the water supply system necessary for the subsistence of the societies that inhabited Sela over time. The system consists of canals, cisterns, and sedimentation basins for the collection, conduction, storage, and preservation of water, mainly from rain. Some of Sela's hydraulic structures may have originated in the Bronze Age (mid-late 2nd mill. BCE), but more secure dating is needed to substantiate this possibility.
... At some localities, the former may be explained by referring to the age of an exposed surface, too young to make the results of stressgoverned weathering visible. In the sandstone inselberg landscapes of south Jordan rock faces exposed by recent rock slope failures lack evidence of cavernous weathering, contrasting with heavily hollowed surfaces beyond the fresh failure scar (Goudie et al., 2002;Migoń and Goudie, 2014). If a timescale of cavern development can be constrained, a tool to establish ages of past slope failures may become available, even if perhaps only a crude dating would be feasible. ...
... The role of large rock-slope failures in the evolution of sandstone rock slopes and escarpments is undoubted, as testified by relevant landform assemblages which include rock fall scars, open clefts, toppled columns and slabs, landslide amphitheatres, block fields, rotated and back-tilted blocks, debris spreads (e.g., Rybář et al., 2006;Forczek, 2008Forczek, , 2009Coltorti et al., 2009;Ward et al., 2011;Migoń and Goudie, 2014;Migoń and Kasprzak, 2016). Occasionally such massive failures are eye-witnessed (Yan et al., 2016). ...
Article
This paper provides a review of recent publications dealing with different issues of sandstone geomorphology, which was long an under-researched theme. Nevertheless, considerable advances have been made recently regarding the origin of various characteristic landforms and landscapes developed in sandstones. The structure of this review reflects the diversity of spatial scales, so that it begins with minor landforms and moves towards regional landscapes, considering both the form and the process. It first focuses on the origin and evolution of mi-croforms on rock surfaces, especially honeycombs and arcades, which have been demonstrated to reflect the distribution of stress within the rock mass and the hydraulic field. A distinction is made between 'organizing' and 'decay' factors, with the latter varying depending on local circumstances, whereas the overarching role of the former explains equifinality. Then the concept of negative feedback between stress and erosion is reviewed, with reference to medium-scale landforms, mainly pedestal rocks and rock arches. In the next part new evidence and ideas about the role of subsurface processes in shaping medium-size and major landforms is presented, with emphasis on chemical decay (arenization), mechanical erosion and sapping. Larger landforms discussed are rock cities and ruiniform relief, canyons and mesas. It is argued that subsurface processes play an important part in the evolution of rock cities and boulder-filled canyons, whereas recent work on residual hills shows that plateau ➔ mesa ➔ butte ➔ pinnacle trajectory is but one possible pathway of geomorphic evolution of tablelands. In the following part a new concept of in situ disintegration of sandstone-capped escarpments is presented as complementary to the widely accepted model emphasizing large scale, often catastrophic mass movements. Finally , recent attempts to use geomorphometry tools to characterize rugged sandstone relief are presented. The paper is closed with an outline of challenges for the future.
... The sandstone weathering patterns in the arid environment creates a striking landscape. This all results in a unique landform that characterizes the area (Migoń and Goudie, 2014). The site is not only strategic in its location, situated on one of the important trading routes linking the Arabian Peninsula with Egypt and the Levant, but also rich in its history which goes back to the Upper Palaeolithic period through to the Roman and Islamic periods up to the present (Cordova et al. 2014, 17). ...
Chapter
Wadi Rum in the south of Jordan was declared in 1998 as a protected area and was inscribed in 2011 on the World Heritage List. It is one of the most visited sites by foreign and local tourists, as statistics of the year 2017 show around 39,000 Jordanians and 139,000 foreigners visiting the site. Despite a long history of occupation and the abundance of archaeological features, the main attractions are related to adventure tourism, as the site is renowned for its natural beauty. The trails starting from the visitor's centre concentrate on few attractions besides of the desert landscape. They thus neglect the local village of Rum, despite its anthropological and historic importance, containing gems such as the Nabatean Temple and Rum Fort. Therefore, a project focusing on enhancing and improving the touristic experience within the Village of Rum was suggested highlighting these historical elements. This project was initiated in 2014 by the Centre for the Study of Natural and Cultural Heritage at the German Jordanian University and the Aqaba Special Economic Zone Authority, which is responsible for the development of Wadi Rum Reserve, to rehabilitate and present the old fort of Wadi Rum and the surrounding area. The project envisions creating a new tourist focal point by transforming the neglected fort into an attraction zone, the core of which is an open-air museum that tells the story of the evolution and history of the area. Using modern technologies and inspired by local materials, the design creates trails evoking Nabatean commerce that will take the visitors on a live trip that stimulates their senses and curiosity. The fort design will also incorporate the local village.
... It was also observed that depending on the density of jointing and the degree of cementation, breakdown of coarse clastic rocks occurs via two distinct pathways. One involves detachment of individual grains or clasts and is termed grain-by-grain disintegration, whereas block-byblock release is an alternative mechanism, typical for more cemented and mechanically stronger rocks (Goudie et al., 2002;Young et al., 2009;Migoń and Goudie, 2014;Young and Wray, 2015;Migoń, 2020). These two pathways produce different shapes of residual landforms. ...
Article
Coarse clastic sedimentary successions cover approximately-one fourth of the continental surface and give rise to distinctive landforms at a variety of scales. Rock-mass strength differences between members of layered successions account for the presence of escarpments, typically capped by thick sandstone or conglomerate beds, usually also with mid-slope cliffs and benches reflecting variable resistance of individual members of the succession. Depending on the dip of strata, two main types of regional landscapes are plateaus and plains, or homoclinal ridges (cuestas), but higher degree of deformation may occur in the vicinity of major faults, resulting in hogback morphology. Medium-scale landforms include residual hills of various types such as mesas and buttes, rock cities and assemblages of ruiniform relief, whereas canyons and slots are common valley forms. Escarpment retreat is usually considered as an overarching concept in geomorphology of layered successions, but it does not seem to be a universal pathway of landscape evolution and even retreat itself may occur in different ways. We propose that juxtaposition of strong and weak rocks in the vertical succession is the viable unifying theme, as it has profound geomorphological implications, influencing processes and patterns of evolution at a variety of spatial scales. However, depending on lithological characteristics, mechanical and hydrogeological properties, dominant processes may vary, explaining considerable landform diversity within tablelands, even though at the grand scale stepped topography becomes a repetitive theme. Synthetic graphical presentation of morphogenetic systems on coarse clastic successions is also presented.
... Rock properties exert a fundamental control on differential weathering of rock surfaces and, hence, on the development of minor landforms within rock masses (Mol and Viles, 2012;Migoń and Goudie, 2014;Young and Wray, 2015). The bedrock of the YNS is composed of the aeolian sandstones of the Luohe Formation, which are homogeneous, thick-bedded, highly porous and permeable. ...
Article
Cavernous weathering is commonly found on sandstone slopes in different environments. Either a single dominant process or polygenetic agents require to be invoked in order to interpret the development. The Yongningshan hill of the central Loess Plateau is representative of cliff dwellings in Northwest China, which is characterized by well-developed cavernous weathering features and provides a good opportunity for the better understanding of sandstone weathering in the Loess Plateau. Multiple methods, including field survey, in-situ rock strength measurement, along with experiments on samples for microscopic observation, element composition and salt chemistry, were employed to investigate the controlling factors of cavernous weathering. The results show that cavern development is different on the four slopes with the western slope hosting massive honeycombs, tafoni and hardened surfaces. The porous and permeable aeolian sandstones are fundamental, because they provide space and pathways for the transportation of water and salt, honeycombs dominantly aligning within the lamination of cross-beds. The environmental factors such as the seasonal wetting and drying cycle, aeolian salt, moisture and water vapor are key factors for the development of cavernous weathering forms. The northern and northwestern wind-blown dust storms have brought abundant salts, the lengthier dry periods of the wetting and drying cycle being beneficial for salt accumulation within caverns, favoring salt weathering.
Article
Full-text available
Several surface investigation techniques, such as X-ray diffraction (XRD), EDX, and optical microscopy, were employed in order to describe the mineral contents in several geomaterials. Space and time resolved optical emission spectroscopy was implemented to analyze the plasma generated by the laser–geomaterial interaction. The values of the plasma parameters (velocity and temperature) were discussed with respect to the nature of the minerals composing the geomaterials and the morphological structure of the samples. Correlations were found between the excitation temperatures of the atomic and ionic species of the plasmas and the presence of calcite in the samples. A mathematical model was built to describe the dynamics in ablation plasma using various mathematical operational procedures: multi structuring of the ablation plasma by means of the fractal analysis and synchronizations of the ablation plasma entities through SL (2R) type group invariance and in a particular case, through self-modulation in the form of Stoler type transformations. Since Stoler type transformations are implied in general, in the charge creation and annihilation processes, then the SL (2R) type group invariance become fundamental in the description of ablation plasma dynamics.
Article
Full-text available
Heavy and clay minerals as tools in solving stratigraphic problems: A case study from the Disi Sandstone (Early Ordovician) and the Kurnub Sandstone (Early Cretaceous) of Jordan
Article
Full-text available
The Stołowe Mountains (SW Poland) represent a unique Central European example of a sedimentary rock stepped tableland in a water divide setting. Sandstone units play a prominent part in the morphology of the massif, acting as cliff formers and supporting extensive plateau levels. High-resolution elevation data acquired from airborne laser scanning allowed us to objectively characterize local relief through selected geomorphometric parameters such as elevation, slope, relief energy, and aspect. In addition, a Topographic Wetness Index was calculated. This constitutes a major advance in relation to the previous, largely qualitative and site-specific observations. In addition, through this detailed geomorphometric approach new facets and features of relief have been revealed and differences between various parts of the massif highlighted. Sandstone escarpments differ in morphology and hence, by inference, in formative processes. Differential retreat by sapping and mass movements is the long-term pathway of geomorphic evolution but along the northern escarpment it seems to have been recently replaced by erosional dissection of plateau rims.
Technical Report
Full-text available
The full report, and associated files, are held by the department. This version provides the Executive Summary, and the list of publications cited in the report. See also the Poster "Karst-like and Ruiniform Features in Sandstones ..." presented to the ASF Conference, 2011
Article
Full-text available
The Golden Gate Highlands National Park (GGHNP) is well known for its impressive sandstone formations. While previous geoscience research in the park has focused on geology, palaeontology, slope forms and the prominent lichen weathering, remarkably little has been written on the diversity and possible origins of sandstone phenomena in the region. The objectives of this study were (1) to present a geomorphological map of prominent and interesting landforms for particular portions of the park and (2) to document the variety of macro- and microscale sandstone formations observed. During field work, we undertook global positioning system measurements to map landforms and, in addition, measured the dimensions of several landform types. A Schmidt hammer was used to conduct rock hardness tests at a variety of localities and lithologies for comparative purposes. We indentified and mapped 27 macro- and microscale sandstone landforms, of which 17 are described in detail. It is demonstrated that for the most part, the landforms are a likely product of surface lithological reactions to a regional climate characterised by pronounced multitemporal temperature and moisture shifts, recently and in the past. However, many of the geomorphological processes producing landforms are controlled by microclimates set up by factors such as macro- and microtopography. CONSERVATION IMPLICATIONS: The GGHNP is best known for its geological, geomorphological and palaeontological heritage. This paper highlights the diversity of sandstone geomorphological phenomena, many of them rare and 'unique' to the region. Not only are these landforms of aesthetic interest to tourists, but they also provide microhabitats for biota. Thus, conservation of biota requires associated conservation of geo-environments where they are established.
Article
In southern Jordan, in the vicinity of Al-Quwayra and Wadi Rum, there is an area of Cambrian/Ordovician sandstones that produces some of the most spectacular desert sandstone relief on Earth. Low angle plains separate large inselbergs, which are characterized by steep cliffs, major alcoves, natural arches, many rockfalls, a lack of talus, and the development of remarkable columnar weathering networks. Data are presented on the morphometry of these weathering phenomena, their Schmidt Hammer hardness values, and their salt chemistry. It is proposed that case hardening and salt weathering are crucial processes in the development of the weathering forms. A discussion is provided on the distribution, age and geotechnical relationships of the rockfalls, together with a description of the ramp slopes that extend from the bases of the cliffs. The absence of talus is a characteristic that the slopes of the area share with many of the sandstone slopes of the Colorado Plateau.
Article
The spectacular relief of the sandstone inselbergs is maintained by an interplay of geological structure and weathering/erosion processes, in that vertical joints and faults provide the foci along which most weathering and erosion take place. There are three major varieties of sandstone breakdown; the first is failure of large rock masses along vertical joints, leading to rockfall. Associated with this process is the mechanical breaking of falling blocks upon impact, in some cases right down to the origjnal sand grains. Rockfall maintains vertical or steep slopes, provided basal talus is removed. The second variety is liberation of small blocks by weathering along closely-spaced joints and bedding planes. Rock prone to this style of erosion tends to be less steep and may have basal slopes buried by rubble. The third variety is grain by grain weathering by solution of cement. This process is the most fundamental, as it not only wears away the surfaces but attacks joints, leading to the processes described above. Grain by grain weathering is slowed or prevented on some surfaces by development of oxide rinds, particularly where run-off is concentrated.These processes result in deposition of debris at slope bases, but in most cases the debris is quickly reduced to sand and removed by wind and water. Relatively clean slope bases allow slopes to retreat parallel to themselves. Where debris collects faster than it is reduced to sana, slope angles tend to decline until they reach the angle of repose of the debris.Differences in structural expression of the various lithological units result in differing erosional characteristics. The Saleb Formation is typified by relatively gentle slopes littered with debris, due to thinly spaced joints. The Ishrin Formation, witll widely spaced vertical joints, is typified by rockfall of large masses. It is the major cliff-former. Grain by grain weathering, influenced by variations in varnish development, has produced spectacular tafoni on some Ishrin cliffs. The Disi Formation is extremely friable and although slopes are relatively gentle they are mostly rubble free. The Disi in many places forms rounded domelike shapes which may be due to exfoliation along pressure-relief joints. The Um Sahm Formation is highly fractured and similar in appearance to the Saleb.Igneous rocks, where exposed below the sandstones, are undergoing chemical weathering, particularly along joints. The results are tors, tafoni, and large amounts of grüss.The desert floor between inselbergs is in some places a bare bedrock surface with an integrated drainage network, and in other places a sand or playa surface. Running water seems to have been a major agent in shaping the floor, but is less important now than in the past. Transportation of sand by wind is common but there is no evidence for significant eolian aggradation or degradation at the present time.A minimum rate of surface retreat by grain by grain weathering is 5 cm./1,000 years, based on weathering ofNabataean ruins. Overall slope retreat should be significantly greater, due to added effects of rockfall and removal of blocks by running water.
Article
In southwestern Jordan a spectacular inselberg landscape has resulted from dissection of Paleozoic sandstones following stripping of Cretaceous/Tertiary carbonates. Erosion of the sandstones was tied to development of the adjacent Dead Sea Rift in two ways: subsidence along the rift axis provided a low base level that facilitated erosion, and faulting associated with the Dead Sea and Red Sea Rifts led to differential erosion and isolation of inselbergs. Most of the erosion took place in and after Miocene time. The major drainage outlet, Wadi Yutm, probably existed throughout development of the landscape, but was temporarily blocked during a normal faulting episode. Following graben-faulting and stream erosion, aggradation of sand and playa sediment created a relatively flat plain above which rise erosional outliers of the sandstones.
Article
The Precambrian shields of the Sahara and Arabia are overlain by a thick laterally extensive Cambro-Ordovician sandstone blanket. This is generally divisible into a lower coarse pebbly cross-bedded facies overlain by a finer-grained facies with a characteristic suite of trace fossils. This paper describes the sedimentology of the Gambro-Ordovician sequence where it crops out in the Southern Desert of Jordan. The lower coarse pebbly facies consists of a complex of channels up to 300 m wide and 15 m deep with occasional shale-filled channels of similar dimensions. Three formations of this facies occur The lowest overlies a mature pediment with residual inselbergs cut in the Precambrian basement. The succeeding two formations have channelled bases. This facies is attributed to three cycles of pedimentation and sedimentation on braided alluvial outwash plains. The overlying facies consists of an alternation of medium grained well sorted sandstones and rare shales. The sandstones are devoid of channelling being composed of laterally extensive tabular-planar cross-bedding. The interbedded shales have sheet geometries, in contrast to the shoestring shaped shales of the facies beneath They consist of laminated silts and microcross-laminated fine sands with a diverse suite of trace fossils. This upper facies is attributed to deposition on a marine shelf by the alternation of migrating sand shoals and tidal flats.