- “Bringing The Past, Into the Future”
- +44 (0) 1204 388754
PRODUCTS BY WEIGHT
BOX SETS
PLASTIC DISPLAY PRODUCTS
PRODUCTS BY WEIGHT
BOX SETS
PLASTIC DISPLAY PRODUCTS
£15.00 ex VAT
Early Cretaceous Environments of the Weald (1996)
by Alastair Ruffell, Andrew Ross & Kevin Taylor
In order for the Guide not to become out-of-date it concentrates on exposures that are likely to remain in their present state for some time, thus some abandoned sites are omitted. The interested geologist will find the locations easily, observe the main features with no trouble, and be able to do this for some years to come.
Out of stock
We ship to all 50 states, Washington DC.
All orders are shipped with a UPS tracking number.
Always free shipping for orders over US $200.
During sale periods and promotions the delivery time may be longer than normal.
Elessi will accept exchanges and returns of unworn and unwashed garments within 30 days of the date of purchase (14 days during the sales period), on presentation of the original till receipt at any store where the corresponding collection is available within the country of purchase.
Your return will usually be processed within a week to a week and a half. We’ll send you a Return Notification email to notify you once the return has been completed.
Please allow 1-3 business days for refunds to be received to the original form of payment once the return has been processed.
Give us a shout if you have any other questions and/or concerns.
Email: contact@mydomain.com
Phone: +1 (23) 456 789
Early Cretaceous Environments of the Weald (1996)
by Alastair Ruffell, Andrew Ross & Kevin Taylor
In order for the Guide not to become out-of-date it concentrates on exposures that are likely to remain in their present state for some time, thus some abandoned sites are omitted. The interested geologist will find the locations easily, observe the main features with no trouble, and be able to do this for some years to come.
Weight | 250 g |
---|
|
|
0% |
|
|
0% |
|
|
0% |
|
|
0% |
|
|
0% |
D-D Landings in Normandy, 1944 (2003)
The only British Guide to the geological controls on the D-Day landings in Normandy. The guide puts into context many of the reasons why the Normandy coast was selected for the invasion, reasons most people are, or were, unaware of. The four itineraries are based on examining the solid (mainly highly fossiliferous Jurassic strata) and superficial (such as Pleistocene loess) geology exposures associated with and adjacent to the main landing areas, Sword, Juno, Gold, Omaha and Utah Beaches, including considering them in terms of water supply, aggregate sources, airfield sites and cross-country movements. A glossary is incorporated.
Out of stock
Dalradian of Scotland
Jack Treagus (2009)
The Dalradian Supergroup of mainland Scotland occupies most of the area generally known as the Grampian Highlands, geographically bounded by the Great Glen Fault to the north and the Highland Border Fault to the south. The Dalradian of Scotland offers the greatest variety of metamorphic rocks to be found in the British Isles. There are sedimentary rocks ranging in composition from limestones and mudstones to conglomerates, often with beautifully preserved sedimentary structures providing evidence of the depositional environments.
Out of stock
The Aberystwyth District (1995)
compiled by M.R.Dobson
The Aberystwyth Grits and Borth Mudstones (Silurian) are magnificently exposed in accessible cliffs along the coastline of Cardigan Bay and are world-famous as classic examples of turbidity current deposition. But the region is also known for the variety of its glacial landforms and modern sedimentary environments . Nineteen itineraries are described in detail, the first eight dealing with the variations in the turbidite fan succession between New Quay in th south and Harp Rock in the north. The rest cover the Dovey Estuary, the Quaternary and solid geology of Cardigan Bay and the Plynlimon area. A glossary is included.
2 in stock
Eastern and Central Jamaica (1995)
by S.K.Donovan, T.A.Jackson, H.L.Dixon & E.N.Doyle
The oldest rocks in Jamaica are Cretaceous with the succession dominated by andesitic volcanic rocks with associated limestones representing an island arc system. The principal features of the geology of the island are described followed by ten itineraries which illustrate at outcrop the variety of the Cretaceous to Recent rocks including granite-like intrusions, volcanic lavas and altered ashes, mineral deposits, highly fossiliferous limestones and shales, and economically important bauxites. Car hire is recommended.
1 in stock
Rockwatch Guide No 1, to the London Clay exposed on the North Shore of The Isle of Sheppey, Kent. The guide is highly informative of the area and also contains clear diagrams to aid the text.
4 in stock
Lanzarote, Canary Islands (2000)
by Trevor Greensmith
This guide is intended for those who are intrigued by the various manifestations of volcanicity and who wish to experience first hand the consequences of such without having to trek long distances in dangerous terrain. All locations in this guide are either roadside or involve walking short distances along tracks.
Out of stock
38. The Plymouth Area (1978) by D.M.Hobson
The five excursions described in this Guide are centred on the city of Plymouth, and although they are mostly concerned with Lower Devonian rocks, details of other important elements in the local Variscan geology are also included. The first three excursions deal with the stratigraphy and structure of various sections across the Dartmouth Antiform, itinerary four with the southern flanks of the Antiform and rocks of the Start Complex, and itinerary five with features exposed inland north of Plymouth.
Out of stock
During the last 16 million years (up to recent times) igneous rocks with a variety of compositions have been extruded and then moved E or W of the rift valley which marks the central line of the Mid-Atlantic Ridge The ice sheets and their associated glaciers formed by the accumulation of snow over hundreds of years, occupy 11% of Iceland. The pressure on water trapped in geothermally heated cavities close to the land surface is occasionally relieved generating Geysers. The itineraries in the Guide provide a representative selection of sites of the above.
Out of stock
Hadrian’s Wall (1997)
Geology of Hadrian’s Wall by G.A.L.Johnson
The geology of Hadrian’s Wall falls naturally into three sectors: in the East the wall is over Upper Carboniferous Coal Measures and Millstone Grit; the Central Section is underlain by Lower Carboniferous intruded by the Great Whin Sill and in the Western sector the Wall crosses the New Red Sandstone. Glacial drift is widespread. All three sectors are described with specific sites in detail.
Out of stock
Watchet and its neighbourhood, Somerset (2006)
A short guide, very suitable for beginners, to the Devonian, New Red Sandstone and Jurassic (Lias) rocks in the vicinity of Watchet. Relatively gentle walks along the foreshore and inland to view exposures, plus the added bonus of examining the usage of local and imported rocks for walls, housing and bridges.
Out of stock
Geology of the Western Front (1999)
by Peter Doyle
Geology and topography of the battlefields of France and Belgium had an important role in determining the character and the outcome of many of the most famous battles. This Guide is intended for all people with an interest in the British sector of the Western Front and, although geological terms are included, they are kept to a minimum and those that are deemed essential are included in a glossary at the end of the guide.
2 in stock
Isle of Arran (1989) 2nd Edition by W.S.McKerrow and F.B.Atkins
The large variety of igneous and sedimentary rocks to be seen on the excellent coastal and island exposures, perhaps excelling any other area in the world has made the Isle of Arran so popular with geologists. The guide has been written assuming a very basic knowledge of geology on the part of the reader. After an extensive introduction to the geology of Arran the six excursions are described together with geological sketch maps. Each excursion can be carried out in seven to eight hours with an indication of a suitable lunch stop!
1 in stock
Reviews
There are no reviews yet.