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Moravian Preservation Master Plan.indb - Society for College and ...

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<strong>Moravian</strong> <strong>College</strong> • <strong>Preservation</strong> <strong>Master</strong> <strong>Plan</strong><br />

Chapter Two<br />

Historic Overview of <strong>Moravian</strong> <strong>College</strong><br />

2.0 Introduction<br />

<strong>Moravian</strong> <strong>College</strong> has a long <strong>and</strong> rich history. Closely<br />

intertwined with the establishment of Bethlehem<br />

<strong>and</strong> <strong>Moravian</strong> theology <strong>and</strong> culture, today’s college<br />

is the descendant of two distinguished <strong>Moravian</strong><br />

educational institutions, which served both men<br />

<strong>and</strong> women over the course of two centuries be<strong>for</strong>e<br />

merging in 1954. The founders of these schools were<br />

also instrumental in the settlement <strong>and</strong> growth of<br />

<strong>Moravian</strong> Bethlehem. Though Bethlehem’s era as<br />

an exclusively <strong>Moravian</strong> settlement is long gone,<br />

<strong>Moravian</strong> <strong>College</strong> <strong>and</strong> its parent schools have<br />

perpetuated some of the <strong>Moravian</strong> faith’s most<br />

cherished educational <strong>and</strong> cultural values into<br />

the present day, <strong>and</strong> kept this legacy relevant to<br />

generations of students.<br />

2.1 Bethlehem: <strong>Moravian</strong><br />

Capital to Industrial Giant<br />

Natural <strong>and</strong> Scenic Qualities of<br />

Bethlehem<br />

The earliest part of Bethlehem, including the<br />

entirety of today’s Priscilla Payne Hurd Campus,<br />

st<strong>and</strong>s atop a bluff overlooking the confluence of<br />

the Lehigh River <strong>and</strong> Monocacy Creek. The site is<br />

part of the Great Valley, a large limestone <strong>for</strong>mation<br />

measuring eight to twelve miles in width, which<br />

curves north into New Jersey <strong>and</strong> south through<br />

Pennsylvania into Maryl<strong>and</strong> <strong>and</strong> Virginia. The<br />

site is part of the Lehigh River drainage area. The<br />

Lehigh River flows eastward to the south of the<br />

bluff, <strong>and</strong> Monocacy Creek flows southward to<br />

the west of the project area (see figure 1-1). Bedrock<br />

beneath the city consists of medium-gray thickbedded<br />

dolomite <strong>and</strong> impure limestone calcareous<br />

siltstone at its base. Subsoil in the area is yellow to<br />

reddish-yellow clay (Gerhardt et al. 2008:4; National<br />

Heritage Corporation 1977:20).<br />

The site chosen <strong>for</strong> the city had a number of<br />

features attractive to the first settlers. Foremost was<br />

a plenteous spring at the base of the bluff, which<br />

would provide water in all seasons <strong>and</strong> was a<br />

primary reason <strong>for</strong> the purchase of this particular<br />

tract. The hillside was wooded with a steep descent<br />

to the river <strong>and</strong> creek. Monocacy Creek at that time<br />

flowed south along the west side of the future city<br />

<strong>and</strong> then turned toward the east, meeting the Lehigh<br />

River southeast of the town site <strong>and</strong> <strong>for</strong>ming a long<br />

east-west peninsula between the two waterways.<br />

On the south side of the Monocacy Creek peninsula<br />

was a <strong>for</strong>d across the Lehigh River. The new town<br />

was sited “some distance from the river” beside an<br />

old Native American trail that extended north <strong>and</strong><br />

west from the <strong>for</strong>d, crossing the peninsula <strong>and</strong> the<br />

Monocacy Creek, <strong>and</strong> running uphill past the new<br />

site (Murtagh 1967:23).<br />

Roots of <strong>Moravian</strong> Faith<br />

<strong>Moravian</strong> Christianity dates back to the fifteenth<br />

century, <strong>and</strong> had two distinct periods: the original<br />

Bohemian church, which was eventually driven<br />

underground, <strong>and</strong> the Renewed Church beginning<br />

in 1722 (Weinlick in Myers 1982:5). <strong>Moravian</strong>ism<br />

began in Bohemia <strong>and</strong> Moravia in central <strong>and</strong><br />

Eastern Europe (figure 2-1). This area was originally<br />

Christianized by the Eastern Orthodox branch of<br />

Catholicism, but eventually Roman Catholicism<br />

became the controlling denomination. Still, the<br />

Christians of these regions felt ties to the Eastern<br />

tradition <strong>and</strong> as such reacted strongly to the<br />

worldly corruption occurring within the Roman<br />

Catholic Church during the 1300s <strong>and</strong> 1400s. John<br />

Hus (born 1369), an instructor at the University of<br />

Prague, helped voice the sentiment that Christian<br />

belief <strong>and</strong> way of life derived from the Bible, not<br />

from the Pope <strong>and</strong> the church leadership hierarchy.<br />

Following his break with the Church, Hus was<br />

condemned as a heretic <strong>and</strong> burned at the stake in<br />

1415. His martyrdom sowed seeds of Protestantism<br />

among his community (Groenfeldt 1976:13).<br />

In the years following the death of Hus, his followers<br />

struggled with different perspectives but could not<br />

create a united community of believers. One faction<br />

separated itself in 1457, <strong>and</strong> was known as the<br />

Unity of the Brethren (Unitas Fratrum). The group’s<br />

primary goal was to avoid further religious conflict<br />

<strong>and</strong> live peacefully, following the teachings of the<br />

New Testament. Despite continued persecution,<br />

the denomination began to grow. During the Thirty<br />

John Milner Associates • October 2009 • Chapter 2 • Historic Overview • 5

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