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Seneca Lake

Seneca Lake

Carved out of glacial movement that began during the Ice Age over two million years ago, the Finger Lakes is the result of ice sheets that last receded and melted approximately 10,000 years ago. Seneca Lake is the deepest (618’ deep below sea level) and one of the two largest in length next to Cayuga Lake.

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Vineyard

VINEYARD INFO

Plant Dates 2014, 2015, 2017, 2018, 2019
Planted Acres 21 (78 total, potential for up to 47 planted acres)
Total planted blocks 4 (blk acres: a – 10; b – 5; c – 5; e – 1)
Vines per acre 1,815 / Spacing 6x4
Rootstocks 3309, so4, Riparia Gloire (rg), Selection Oppenheim (so4), 101-14
Variety & Clonal Selection Riesling (198, 239, 90, 110, HJW (Hermann J. Wiemer), 22.1)

Soils

VINEYARD INFO

60% blue slate from Mesozoic time period

25% glacial till Characterized as boulders and pebble rock by the Ice Age

15% limestone glacial shale Found sporadically, created from Mesozoic time period up to present day

Farming

Seneca Lake

We are vigilant in our stewardship of the land and engaged in labor-intensive, hand-farming methods year-round to grow fruit to the highest quality. The up to 55-degree gradient requires specialized equipment and erosion prevention measures such as no tilling or exposed soils and year-round cover crop.
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Discovery & Development

Seneca Lake

After years of searching around the Finger Lakes, Paul and David ultimately concentrated their efforts on Seneca Lake and found a property with similar attributes to those found in the famed Mosel region. Previously planted to native Labrusca varieties in the late 1800’s, the property started to become overgrown in the 1930’s after farming was abandoned. Old cedar posts and wire trellising were found in the wooded areas, along with small terraces that allowed horses to work the original vineyard.

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Seneca Lake

Carved out of glacial movement that began during the Ice Age over two million years ago, the Finger Lakes is the result of ice sheets that last receded and melted approximately 10,000 years ago. Seneca Lake is the deepest (~618’ deep) and one of the two largest in length next to Cayuga Lake.

Estate

Situated on the southeastern banks of Seneca Lake, the property was acquired in 2013 and started being converted to Riesling one year later. The vineyards are planted to high density and one of the first in the area to run up and down slope similar to those of the Mosel region.

Discovery & Development

After years of searching around the Finger Lakes, Paul and David ultimately concentrated their efforts on Seneca Lake and found a property with similar attributes to those found in the famed Mosel region. Previously planted to native Labrusca varieties in the late 1800’s, the property started to become overgrown in the 1930’s after farming was abandoned. Old cedar posts and wire trellising were found in the wooded areas, along with small terraces that allowed horses to work the original vineyard.

Farming

We are vigilant in our stewardship of the land and engaged in labor-intensive, hand-farming methods year-round to grow fruit to the highest quality. The up to 55-degree gradient requires specialized equipment and erosion prevention measures such as no tilling or exposed soils and year-round cover crop.

Hillick & Hobbs Estate is certified under New York Sustainable Winegrowing.

The estate revives the Hobbs family legacy of growing grapevines in upstate New York.