scholarly journals WHICH SIDE OF THE TREE DOES PHLŒOTRIBUS LIMINARIS ATTACK?

1893 ◽  
Vol 25 (4) ◽  
pp. 111-112
Author(s):  
F. M. Webster
Keyword(s):  
New York ◽  
Lake Erie ◽  
The South ◽  
South Shore ◽  
Old Trees

Recently, while studying the habits of this beetle in the peach orchards of Catawba Island, on the south shore of Lake Erie, I was surprised to observe that the fall attack had invariably been made on the east or southeast side—which is here the land side of the trees—and old trees, where the bark of the trunks was very rough, were more seriously affected. On mentioning the fact of this apparent discrimination in point of attack to my friend Dr. D. S. Kellicott, he recalled that the same phenomenon occured about Buffalo, New York.

WATER QUALITY MONITORING IN THE SOUTH SHORE ESTUARIES OF LONG ISLAND, NEW YORK

2018 ◽  
Author(s):  
Rebeka Smith ◽  
◽  
Thomas Badamo ◽  
David J. Barclay ◽  
Devorah Crupar ◽  
...  
Keyword(s):  
Water Quality ◽  
New York ◽  
Long Island ◽  
Water Quality Monitoring ◽  
Quality Monitoring ◽  
The South ◽  
South Shore

scholarly journals A PROLONGED SEASON OF OCCURRENCE FOR SCHISTOCERCA AMERICANA

1899 ◽  
Vol 31 (2) ◽  
pp. 28-28
Author(s):  
F. M. Webster
Keyword(s):  
Lake Erie ◽  
The State ◽  
Schistocerca Americana ◽  
The South ◽  
Northern Portion ◽  
South Shore

At Wooster, Ohio, this species was observed in the fieds on May 26, and at Alliance, nearly due east, on October 24, while at Bridgeport, in the extreme eastern central part of the State, it was found, active, on November 4, all during 1898. It appears to have been more numerous of late in the vicinity of the south shore of Lake Erie than elsewhere in the northern portion of the State, and more abundant than I have formerly observed it in the same latitude in Indiana and Illinois.

scholarly journals THE MOTION OF SEDIMENT ALONG THE SOUTH SHORE OF LAKE ERIE

2000 ◽  
Vol 1 (4) ◽  
pp. 8
Author(s):  
Howard J. Pincus
Keyword(s):  
Lake Erie ◽  
The South ◽  
Small Areas ◽  
Local Characteristics ◽  
South Shore

Much of Lake Erie' s southern shoreline displays fairly uniform properties with respect to shore processes. However, detailed studies of selected stripe of shore areas often reveal characteristics which are so distinctive that problems of control require special attention to local characteristics. The purpose of this paper is to present some generalizations and some detailed comments on the motion of sediment along the south shore of Lake Erie, to outline the results of some detailed studies of small areas, and to evaluate the types of evidence used in such studies.

Interpretation of lithofacies of the Ashtabula Till along the south shore of Lake Erie, northeastern Ohio

1997 ◽  
Vol 34 (1) ◽  
pp. 66-75 ◽  
Author(s):  
John P. Szabo ◽  
Pierre W. Bruno
Keyword(s):  
Lake Erie ◽  
Carbonate Content ◽  
Mass Wasting ◽  
The South ◽  
Depositional History ◽  
Waves And Currents ◽  
History Of ◽  
South Shore ◽  
Late Wisconsinan ◽  
Wave Erosion

The final advance of the Erie lobe into Ohio during the Port Bruce Stade of the Late Wisconsinan deposited the Ashtabula Till. Wave erosion and mass wasting along the south shore of Lake Erie show that the Ashtabula Till consists of laterally traceable lithofacies, which are used to determine the depositional history of the Ashtabula Till. At each section, lithofacies sequences are divided into two sub-sequences, each consisting of massive, matrix-supported diamicton (Dmm) overlain by stratified, matrix-supported diamicton (Dms). Some Dmm are sheared (Dmm(s)) and are interpreted as lodgement till, whereas other Dmm and Dms were deposited as melt-out till. Some sections contain lenses of fines (Fm and Fl), current-reworked diamictons (Dmm(c) and Dms(c)), and resedimented diamictons (Dmm(r) and Dms(r)). The two sub-sequences represent two advances of Ashtabula ice that deposited the Euclid and Painesville moraines about a kilometre apart. During and after recession of the Ashtabula ice, waves and currents in Lake Maumee and its successors reworked outwash and diamictons to form the lake plain. The texture of Dmm(s) is significantly different from that of most other diamictons, and Dmm has the smallest carbonate content of all diamictons. Analysis of the variations in texture and composition among lithofacies provides additional evidence of the effectiveness of lithofacies logging in interpretation of glacial processes.

scholarly journals CONSTRUCTION OF A BREACH CLOSURE IN A BARRIER ISLAND

1982 ◽  
Vol 1 (18) ◽  
pp. 75
Author(s):  
M.J. McCarthy ◽  
E.J. Schmeltz ◽  
G.R. Lehan
Keyword(s):  
New York ◽  
Public Safety ◽  
Long Island ◽  
Barrier Island ◽  
Environmental Concerns ◽  
The South ◽  
Winter Storm ◽  
Barrier Beach ◽  
South Shore

A breach was opened in the barrier beach along the south shore of Long Island, New York during a winter storm in January, 1980. Due to public safety and environmental concerns, a contract to close the breach using sand fill was awarded to a local contractor. This paper discusses the evolution of the construction procedures developed to allow the contractor to successfully complete the project on schedule and on budget.

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