IAPETUS SEABED DEPOSITS

Donald Kenney (donaldkenney@gmail.com)
Last Update: Thu Sep 1 07:37:33 2016



Introduction

Having covered the Northeasternmost terranes in the US and Canada -- Meguma in Southeast Nova Scotia, Avalonia strung out from Newfoundland to South Carolina and a Late Paleozoic-Early Mesozoic Maritime Cover terrane deposited atop mostly Avalonian rocks in the Canadian Maritimes and South East New England, we will now move inland to the next terrane. These are what remains of the deep water portion of the Iapetus ocean that once separated North America (Laurentia) from Avalonia.

Terminology

The terminology for Eastern North American rocks originating in the Early Paleozoic Iapetus Sea is extraordinarily confused. For now, suffice it to say that I am considering the Iapetus sea bottom for purposes of these web pages to be composed of three "terranes". On the East is Avalonia and its associated near shore deposits. Avalonia was a long, narrow, continent that appended itself to Paleozoic North America (Laurentia) around 300 million years ago. On the West are rocks deposited along the continental margin of Laurentia (North America) in the Early Paleozoic. I have called these the Taconic-Laurentian Margin Terrane. In between is what I am calling the Iapetus Terrane -- a jumble of seabottom and volcanic rocks derived from deep ocean bottoms, volcanic island arcs, temporary basins formed adjacent to the island arcs, and other deposits. The Triassic Basins, parts of the Maritime Cover terrane, and isolated more recent deposits are pasted on top of the Iapetus sea bottom rocks in places

Background

Sometime before 600 million years ago almost all the continental rock on the planet collected itself into a single "supercontinent" that geologists call Rodinia. Rodinia is not to be confused with the much younger supercontinent of Pangea. Pangea assembled itself about 300 million years ago and broke up roughly 200 million years ago. About 600 million years ago, rifts developed in Rodinia. It fractured into as many as eight fragments. One of these fragments consists of the rocks underlying most of North America. It is called Laurentia. A second fragment included much of what are now Africa, South America, Australia, and Antarctica. It was called Gondwana.

Laurentia and Gondwana were adjacent parts of Rodinia. The rift between them opened and eventually became a full fledged ocean -- the Iapetus Sea. Shortly after the Iapetus started to open, a rift developed in Gondwona that calved a long narrow strip of continental rock called Avalonia into the Iapetus. As time passed, the ocean between Laurentia and Avalonia ceased to widen. One of more subduction zones appeared where surface rocks were sucked into the Earth, and the Iapetus started to close. Eventually, it closed completely folding many hundreds of kilometers of sea bottom into a confused jumble of rocks that can easily be driven across in a few hours.

The cycle of an ocean opening and subsequently closing again is called a Wilson Cycle and is apparently fairly common. The rocks between the nearly four billion year old sediments of the Northwest territories and the relatively young rocks of the St Lawrence River Valley have been interpreted as being the result of a number of Wilson Cycles slowly building Laurentia by a series of fractures, seas opening, seas closing, and a new fracture developing a few hundred kilometers outboard of the previous fracture.

During the opening phase, there was presumably a mid-ocean ridge laying down lava on both sides that became the floor of the Iapetus Sea. Once the opening phase ceased, subduction zones developed along which the Iapetus Sea bottom was sucked into the Earth's mantle. When the material being sucked into subduction zones melts it tends to rise, creating arcs of volcanoes similar to those seen today off the East coast of Asia. These "island arcs" are often fringed by forearc and backarc basins that quickly fill with material eroded from the island arc volcanoes as well as the continents fringing the contracting ocean. These arcs may fill completely and turn into low lying land.

A variety of rock types can be found in these seafloor/basin/arc volcano complexes. What they have in common is that they are rarely very rich in fossils. To further exacerbate the situation as the seas close, the rocks are folded and overthrust in complex patterns. Thousands of kilometers of seafloor may eventually be lost to subduction and erosion. Further some of the rocks exposed in these belts may have been subducted, altered by heat and pressure, then brought back to the surface. Sorting out the provenance and nature of the rocks and the interrelationships of rocks of the same age is a huge job that has only just been started.

The Rocks

Newfoundland

Newfoundland geology was described by Sir Charles Murray head of the Newfoundland Geologic Survey in the 19th Century. He defined a number of zones of rocks deposited in strips running Northeast to Southwest parallel to the West coast of Newfoundland. Some of these zones have survived into modern usage sometimes a bit mangled. The Avalon zone on the East is described here as the Avalon Terrane. The Humber Zone on the West will be described along with the other Taconic-Laurentian Margin rocks. The original Dashwoods, Notre Dame, Dunnage, Gander, Exploits, Zones are usually combined into two zones. The Dunnage zone found East of the Humber zone consists of obvious deep sea bottom sediments -- volcanics and deep water sediments. It is split by the Red Indian Line which is thought to represent a major divide between surviving rocks from the Eastern and Western Iapetus seabottoms. The Gander zone further East consists of "clastics" -- sandstones and shales -- intruded by igneous rocks such as granite and of metamorphosed rocks of various sorts. It is separated from the Dunnage Zone by the Reach Fault. Since granite is a rock typical of continental volcanic activity rather than deep sea vulcanism it is thought that Avalonian continental rock underlies the Gander rocks at depth. Other nomenclature is used by various authors. Being clairvoyance deprived, I will not attempt to describe the nomenclature and geology further.

The Dunnage-Gander rocks contain a few fossils. Enough to demonstrate that they are early Paleozoic and are of marine origin. Some Silurian fossils are found near Glenwood.

Newfoundland

Age Dunnage (Notre Dame) Dunnage (Exploits) Gander
Carboniferous Maritime Cover Terrane
Devonian (intrusives)
Silurian Mimac lake, Cape St John Group Indian Islands Group, Botwood Group
Ordovician (intrusives),Snooks Arm,Flat Water Pond Wild Bight Group*, Davidsonville Group, Badger Group
(Ophiolites) Victoria Lake Supergroup Indian Bay-Big Pond
Cambrian Fleur de Lys Supergroup Victoria Lake Supergroup Jonathans Pond

*The Wild Bight Group consists of five formations -- oldest to youngest -- Seal Bay Brook, Side Harbour, Omega Point, Sparrow Cove, Pennys Brook

New England, Quebec and New Brunswick

In New England, the rocks not belonging to younger "cover terranes" such as the Triassic Basin rocks resemble the Dunnage Zone of Newfoundland to some extent. Rock types are more diverse as they include sediments apparently laid down in shallow waters adjacent to volcanic island arcs as well as some Devonian deposits laid down in shallow basins or in lowlands remaining after the basins filled with sediment. I have quite arbitrarily placed the "Dunnage-Humber" boundary at roughly the Easternmost occurrences of well preserved, shallow water, Laurentian fossils even though in some cases, these manage to be somewhat East of regions of what are clearly continental slope deposits and in other cases regions of fairly strongly metamorphosed rocks exist to the West of my boundary.

A few outcrops of Ordovician and Silurian rocks are found in Maine. Devonian marine fossils and plants are found in basins in the central part of the state.

A few Silurian and Devonian fossils are found in a strip of mildly altered sandstones and limestones along the Connecticut River from Bernardston, MA to and beyond Littleton, NH. Graptolites are found at a number of localities in Northern and Central Vermont.

In Quebec, Dunnage rocks are confined to a narrow, largely unfossiliferous, strip along the borders of New Brunswick, Maine, New Hampshire, and Vermont. At least one Ordovician and one Devonian outcrop have a recognizable fossils

In New Brunswick the Northwestern third of the province is covered with Paleozoic rocks similar those of Maine. A relatively narrow strip on the Southeast side of this belt is mapped as Dunnage and Gander rocks with the beds further Northwest being Silurian and Devonian sediments. The Southeast portion of the province is covered with Maritime Cover Terrane and Avalonian.

For the present, I am assuming that Ordovician and older rocks in New Brunswick are Dunnage-Gander or Avalonian and that Silurian or later rocks are Avalonian or questionably Dunnage. Many authors would disagree and possibly allocate Silurian/Devonian rocks in Northwest New Brunswick to the Humber zone of Laurentian Margin rocks.

New Brunswick

Age Humber(?) and Dunnage Formations
Carboniferous Maritime Cover Terrane
Devonian Gaspe Sandstone
Gaspe
Escuminac
Fleurant
Pirate Cove
Devonian La garde
Silurian Gascons,IndianPoint,Roncelles
Sayabant
Val-Brillant
Awantjish,Burnt Jam Brook,Sources
White Head
Ordovician Pabos
Garin

-- Rocks above here are probably Humber Zone? ------
Arsenault
(Opiolitic melanges )
Cambrian Murphy Creek
bold=fossiliferous italic=calcareous ()=largely volcanic

Northern Maine

Age Formations (West) Formations (East)
Mississippian Miscellaneous intrusives Miscellaneous intrusives
Devonian Upper Mapleton
Devonian Middle Miscellaneous intrusives Miscellaneous intrusives
Devonian-Lower Tomhegan Trout Valley
(unnamed)
Tarratine Mantagammon
Seboomook
Silurian-Upper Dagett Ridge Allsbury,Perlham, Kellyland,Smyrna Mills
Hardwood Mountain
Lobster Lake
Silurian-Middle Chesuncook
Maple Mountain Frenchville
Ordovician Pyle Mountain
Rockland
(Dunn Brook, Nine Lake,Hove) Penobscot
Battie
(Kennebec) (Shin Brook)
Ellsworth
Cambrian Grand Pitch
bold=fossiliferous italic=calcareous ()=largely volcanic

New Hampshire-Western Maine

Age Formations (West) Formations (East)
Jurassic?/Cretaceous? (unnamed) (unnamed )
Devonian Waits River,(Putney),Littleton Sharpleigh,Towow,Littleton
Gile Mt,(Putney)Littleton Sharpleigh,Rindgemere,Littleton,Hildreth
Erving,(Putney)Littleton Sharpleigh,Gonic,Littleton,Seboomook
Merrimack,Berwick,Madrid,Vassalboro
Silurian Berwick,Merrimack Merrimack,Berwick,Casco Bay, Small Falls
Fitch,Eliot,Merrimack Merrimack,Eliot,Perry Mt,Waterville
Mayflower Hill
Clough,Kittery,Merrimack Merrimack,Kittery,Rangeley
Ordovician |(intrusives) (intrusives)
Partridge,Dixville Dixville
(Ammonoosuc) (Rye)
Albee Albee
Rye
Aziscomos Aziscomos
bold=fossiliferous italic=calcareous ()=largely volcanic

Central and Eastern Vermont

Age Formations
Jurassic?/Cretaceous? (unnamed)
Devonian Upper (unnamed)
Devonian Waits River,(Putney),Littleton
Gile Mt,(Standing Pond),Littleton
Northfield
Shaw Mt
Silurian ???
Clough
Ordovician |(intrusives)
Missisquoi
Cambrian Ottauquechee
bold=fossiliferous italic=calcareous ()=largely volcanic

Western Massachusetts and Western Connecticut

Age Formations
Triassic Newark Supergroup
Devonian (unnamed)
Devonian Erving,Littleton,Mt Pisgah,Brimfield?
Waits River,Littleton,Brimfield?
Silurian Goshen,Littleton,Brimfield?,Hamilton Reservior
Russell Mt, Brimfield?
Clough,Bigelow Brook
Hebron, Southbridge
Wepawaug
Ordovician (intrusives)
Wallomsac,Cobble Mt,Partridge,Paxton,Hartland
Wallomsac,(Hawley),(Ammonoosuc), Straits
Wallomsac,Moretown,Collinsville
(Middletown), Tatnic Hill
Stockbridge,Rowe/Waterbury/Hartland,(Monson),(Mamcoke),(Quinebaugh)
Stockbridge,Rowe/Waterbury/Hartland,New London
Stockbridge,Rowe/Waterbury/Hartland,Savin,Glastonbury
Cambrian Hoosac,Waramaug
(Unnamed)
Everett,Cavendish,Plainfield
bold=fossiliferous italic=calcareous ()=largely volcanic {} = intrusives,deep sea metamorphics

Mid Atlantic states

South and West of the Hudson River, there is probably a wide strip of Dunnage zone rocks arcing down toward Alabama. But the Eastern part of it is covered with Cretaceous and Tertiary sediments of the Atlantic Cover Terrane. The rocks exposed West of these relatively young sediments and East of the occasionally fossiliferous Taconic-Laurentian Margin Terrane are generally fairly deformed, non-fossiliferous and in large part buried under Triassic basin rocks. There are possibly fossil exposures in the Southern part of this region where it is broader. The Dunnage zone roughly corresponds to the Piedmont region between the Appalachians and the coastal lowlands. The boundary between Humber rocks and Laurentian rocks appears to swing inland in the Southern Appalachians and it would possibly not be surprising to see the Humber-Dunnage boundary swing West as well. In the Carolinas, the Carolina Terrane exposed on the East side of the Piedmont is thought -- on the basis of a few fossils -- to be Avalonian

Some of the formations listed below may belong in the Taconic-Laurentian margins Terrane and vice versa -- especially in Southeast Pennsylvania and Georgia where the sources I have examined so far do not differentiate the two.

Mid Atlantic States-Southeast Coast

Age Formations
Cretaceous-Tertiary Atlantic Margin Cover
Triassic Newark Supergroup
Undifferentiated Lower Paleozoic (Devonian-Cambrian) Peach Bottom
Arvonia
Cardiff
Irvington Grove
Virgilina Tomstown
Virgilina Urbana
Undifferentiated Late Proterozoic Sediments Virgilina Sugarloaf Mt
Libertytown
Catoctin Sams Creek
Swift Run Wakefield
Silver Run
Liamsville
Lynchburg
Marburg
Wilmington-Wissahickon
Cockeysville
Setters
Baltimore Gneiss Baltimore Gneiss
bold=fossiliferous italic=calcareous ()=largely volcanic {} = intrusives,deep sea metamorphics

Formations in US largely based on American Association of Petroleum Geologists Geological Highway Maps

Localities

No recommended localities. Fossils are uncommon in most of the Dunnage/Gander rocks and most seem not terribly interesting except to the extent that they allow some formations to be dated. Some of the Silurian and Devonian beds of Northwest New Brunswick may be an exception as fossils seem perhaps to be more abundant, more diverse, and better preserved there.

Maps and Figures

Geologic Maps


Newfoundland Island Map http://www.nr.gov.nl.ca/mines&en/geosurvey/maps/nf.pdf Detailed maps http://www.nr.gov.nl.ca/mines&en/geosurvey/maps/nl/


New Brunswick Province map http://www2.gnb.ca/content/gnb/biling/en.html


Quebec -- So far, I have not located a province scale bedrock geology map of Quebec


Maine [State map (Simplified) ttps:web.archive.org/web/*dacf/mgs/pubs/online/bedrock/bedrock11x17.pdf ttps:web.archive.org/web/*dacf/mgs/pubs/online/bedrock/bedrock11x17.pdf]


New Hampshire State map http://geology.about.com/library/bl/maps/n_statemap_NH800.htm


Vermont State map http://www.anr.state.vt.us/DEC/geo/centmap.htm


Massachusetts State map (simplified) http://geology.about.com/library/bl/maps/blmassachusettsmap.htm State map http://www.geo.umass.edu/stategeologist/frame_maps.htm


Rhode Island State map http://geology.about.com/library/bl/maps/blrhodeislandmap.htm


Connecticut State maps http://web.archive.org/web/20120306154657/http://www.wesleyan.edu/ctgeology/images/CtGeoMap_big.jpg--------------------------- New York Generalized Bedrock Geology of NY

Overview of NY Geology


New Jersey Simplified map of NJ

Index to online geology maps of New Jersey


Pennsylvania Simplified map of PA

Digital Geologic map of Pennsylvania


Maryland Geologic Map


Delaware Links to Delaware Geologic Maps


Virginia


North Carolina Generalized map

Access to detailed maps


South Carolina


Georgia High Resolution map


Alabama


Formations

See Rocks


References


Copyright 2006-2012 Donald Kenney (Donald.Kenney@GMail.com). Unless otherwise stated, permission is hereby granted to use any materials on these pages under the Creative Commons License V2.5.

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